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class="ds2-5-heading-sans-serif-xs">Uploads</h2></div><div class="documents-container backbone-social-profile-documents" style="width: 100%;"><div class="u-taCenter"></div><div class="profile--tab_content_container js-tab-pane tab-pane active" id="all"><div class="profile--tab_heading_container js-section-heading" data-section="Papers" id="Papers"><h3 class="profile--tab_heading_container">Papers by Patrick Redmond</h3></div><div class="js-work-strip profile--work_container" data-work-id="4938012"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/4938012/Closure_to_Solute_Breakthrough_Curves_for_Processed_Kaolin_at_Low_Flow_Rates_by_Charles_D_Shackelford_and_Patrick_L_Redmond"><img alt="Research paper thumbnail of Closure to “Solute Breakthrough Curves for Processed Kaolin at Low Flow Rates” by Charles D. Shackelford and Patrick L. Redmond" class="work-thumbnail" src="https://attachments.academia-assets.com/49545275/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/4938012/Closure_to_Solute_Breakthrough_Curves_for_Processed_Kaolin_at_Low_Flow_Rates_by_Charles_D_Shackelford_and_Patrick_L_Redmond">Closure to “Solute Breakthrough Curves for Processed Kaolin at Low Flow Rates” by Charles D. Shackelford and Patrick L. Redmond</a></div><div class="wp-workCard_item"><span>Journal of Geotechnical Engineering</span><span>, 1996</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="81f0c055ffe31fc903341bee13b7e38b" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":49545275,"asset_id":4938012,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/49545275/download_file?st=MTczMjgzMzQzOCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="4938012"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="4938012"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 4938012; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=4938012]").text(description); $(".js-view-count[data-work-id=4938012]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 4938012; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='4938012']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 4938012, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "81f0c055ffe31fc903341bee13b7e38b" } } $('.js-work-strip[data-work-id=4938012]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":4938012,"title":"Closure to “Solute Breakthrough Curves for Processed Kaolin at Low Flow Rates” by Charles D. 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="4938011"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/4938011/Solute_Breakthrough_Curves_for_Processed_Kaolin_at_Low_Flow_Rates"><img alt="Research paper thumbnail of Solute Breakthrough Curves for Processed Kaolin at Low Flow Rates" class="work-thumbnail" src="https://attachments.academia-assets.com/49545288/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/4938011/Solute_Breakthrough_Curves_for_Processed_Kaolin_at_Low_Flow_Rates">Solute Breakthrough Curves for Processed Kaolin at Low Flow Rates</a></div><div class="wp-workCard_item"><span>Journal of Geotechnical Engineering</span><span>, 1995</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="37a157caf1f18399b433ef9930572c7f" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":49545288,"asset_id":4938011,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/49545288/download_file?st=MTczMjgzMzQzOCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="4938011"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="4938011"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 4938011; 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="4938008"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/4938008/Hazard_Analysis_and_Validation_Metrics_Framework_for_System_of_Systems_Software_Safety"><img alt="Research paper thumbnail of Hazard Analysis and Validation Metrics Framework for System of Systems Software Safety" class="work-thumbnail" src="https://attachments.academia-assets.com/49545341/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/4938008/Hazard_Analysis_and_Validation_Metrics_Framework_for_System_of_Systems_Software_Safety">Hazard Analysis and Validation Metrics Framework for System of Systems Software Safety</a></div><div class="wp-workCard_item"><span>IEEE Systems Journal</span><span>, 2010</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Safety-critical software-intensive systems of systems require rigorous verification and validatio...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Safety-critical software-intensive systems of systems require rigorous verification and validation to ensure that they function as per requirements. Unlike verification, validation is typically an ill-defined activity for software development. This paper presents a well-defined validation metrics framework which uses hazard analysis, and the derived software requirements for mitigating the identified hazards, as proxies in gauging the sufficiency of the software safety requirements early in the software development process. Moreover, traditional hazard analysis techniques are insufficient to deal with the complexity and size of systems of systems. This paper examines the nature and types of hazards associated with systems of systems and presents a new technique for analyzing one type of emergent hazard known as an interface hazard.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="1aa25b245cffac3f8c7aacc974db9f9b" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":49545341,"asset_id":4938008,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/49545341/download_file?st=MTczMjgzMzQzOCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="4938008"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="4938008"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 4938008; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=4938008]").text(description); $(".js-view-count[data-work-id=4938008]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 4938008; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='4938008']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 4938008, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "1aa25b245cffac3f8c7aacc974db9f9b" } } $('.js-work-strip[data-work-id=4938008]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":4938008,"title":"Hazard Analysis and Validation Metrics Framework for System of Systems Software Safety","translated_title":"","metadata":{"abstract":"Safety-critical software-intensive systems of systems require rigorous verification and validation to ensure that they function as per requirements. 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Such systems can i...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The next generation of military capabilities will hinge on systems of systems. Such systems can introduce emergent hazards that must be adequately dealt with before the system of systems can be employed. Traditional hazard analysis techniques do not address the complexity and size of systems of systems. In this paper we describe a technique for conducting interface hazard analysis for systems of systems. 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At Bingham, we see no change in the style of wall-rock alteration associated with the ... C, ...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">... At Bingham, we see no change in the style of wall-rock alteration associated with the ... C, during the late Q2 quartz deposition in equilibrium with K-feldspar + biotite, was the ... of an intrusion-centered hydrothermal system: Far SoutheastLepanto porphyry and epithermal Cu-...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="4938005"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="4938005"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 4938005; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=4938005]").text(description); $(".js-view-count[data-work-id=4938005]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 4938005; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='4938005']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 4938005, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=4938005]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":4938005,"title":"Copper deposition by fluid cooling in intrusion-centered systems: New insights from the Bingham porphyry ore deposit, Utah","translated_title":"","metadata":{"abstract":"... 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="4938004"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/4938004/Copper_deposition_during_quartz_dissolution_by_cooling_magmatic_hydrothermal_fluids_The_Bingham_porphyry"><img alt="Research paper thumbnail of Copper deposition during quartz dissolution by cooling magmatic–hydrothermal fluids: The Bingham porphyry" class="work-thumbnail" src="https://attachments.academia-assets.com/49545303/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/4938004/Copper_deposition_during_quartz_dissolution_by_cooling_magmatic_hydrothermal_fluids_The_Bingham_porphyry">Copper deposition during quartz dissolution by cooling magmatic–hydrothermal fluids: The Bingham porphyry</a></div><div class="wp-workCard_item"><span>Earth and Planetary Science Letters</span><span>, 2005</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="631ace84a72ef7693efd2b4fa8f4dd48" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":49545303,"asset_id":4938004,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/49545303/download_file?st=MTczMjgzMzQzOCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="4938004"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="4938004"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 4938004; 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href="https://www.academia.edu/4938003/The_Bingham_Canyon_Porphyry_Cu_Mo_Au_Deposit_I_Sequence_of_Intrusions_Vein_Formation_and_Sulfide_Deposition"><img alt="Research paper thumbnail of The Bingham Canyon Porphyry Cu-Mo-Au Deposit. I. Sequence of Intrusions, Vein Formation, and Sulfide Deposition" class="work-thumbnail" src="https://attachments.academia-assets.com/49545374/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/4938003/The_Bingham_Canyon_Porphyry_Cu_Mo_Au_Deposit_I_Sequence_of_Intrusions_Vein_Formation_and_Sulfide_Deposition">The Bingham Canyon Porphyry Cu-Mo-Au Deposit. I. Sequence of Intrusions, Vein Formation, and Sulfide Deposition</a></div><div class="wp-workCard_item"><span>Economic Geology</span><span>, 2010</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="ec644ccecddc645af1f62db92fd390f8" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":49545374,"asset_id":4938003,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/49545374/download_file?st=MTczMjgzMzQzOCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="4938003"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="4938003"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 4938003; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=4938003]").text(description); $(".js-view-count[data-work-id=4938003]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 4938003; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='4938003']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 4938003, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "ec644ccecddc645af1f62db92fd390f8" } } $('.js-work-strip[data-work-id=4938003]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":4938003,"title":"The Bingham Canyon Porphyry Cu-Mo-Au Deposit. I. Sequence of Intrusions, Vein Formation, and Sulfide Deposition","translated_title":"","metadata":{"grobid_abstract":"The Bingham Canyon porphyry copper-gold-molybdenum deposit is one of the largest and highest-grade porphyry orebodies in the world. This study focused on the northwest side of the deposit where quartz monzonite porphyry (QMP), the first and largest porphyry intrusion, hosts the bulk of the high-grade copper-gold ore (\u003e1.0% Cu, \u003e1.0 ppm Au). The north-northeast-trending, high-grade zone had pre-mining dimensions of 1,500 m strike, \u003e300 m vertical, and 500 m width and contained more than 500 million tonnes (Mt) of ore associated with potassic alteration and abundant quartz veins. The lack of superimposed sericitic alteration yielded ideal exposures in which to study the early, high-temperature stages of ore formation, a style of mineralization that in many porphyry deposits represents the major period of copper introduction.","publication_date":{"day":null,"month":null,"year":2010,"errors":{}},"publication_name":"Economic Geology","grobid_abstract_attachment_id":49545374},"translated_abstract":null,"internal_url":"https://www.academia.edu/4938003/The_Bingham_Canyon_Porphyry_Cu_Mo_Au_Deposit_I_Sequence_of_Intrusions_Vein_Formation_and_Sulfide_Deposition","translated_internal_url":"","created_at":"2013-10-30T07:37:56.283-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":6486462,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":49545374,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/49545374/thumbnails/1.jpg","file_name":"gsecongeo.105.1.4320161012-11940-nyt2kg.pdf","download_url":"https://www.academia.edu/attachments/49545374/download_file?st=MTczMjgzMzQzOCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"The_Bingham_Canyon_Porphyry_Cu_Mo_Au_Dep.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/49545374/gsecongeo.105.1.4320161012-11940-nyt2kg-libre.pdf?1476275298=\u0026response-content-disposition=attachment%3B+filename%3DThe_Bingham_Canyon_Porphyry_Cu_Mo_Au_Dep.pdf\u0026Expires=1732837038\u0026Signature=OVHd2cJ4i00LqE~4E9RDXzvHouqVXm8ecT8G4THxdvqJavpUFH9GMk7LaUJvxSLQnASwlnliqYo48mm~Z99STm6RsHcxPX7L93Jc9ZG--YKD0MQPBjURX5pr-0PvfpjAcioCexuIdusvL3ysVWz40IVnsXAwhnr~pDcmY5PUlVEpR1brM7kQfVbMDLVhWR7qqHDhecxwKml0VMagqBWZAYg-51vu2dVHD4UEMzdKLFb3DJf3EIbV2iIHfyV0cDoXgSo6Uh83um70FchJkPrPo-SfwLMk~mqmg8YctFe6jMC-PqKQXnFvWwWeZcyY-K5WazNe3pSRg4HBedtpx~BUoQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"The_Bingham_Canyon_Porphyry_Cu_Mo_Au_Deposit_I_Sequence_of_Intrusions_Vein_Formation_and_Sulfide_Deposition","translated_slug":"","page_count":26,"language":"en","content_type":"Work","owner":{"id":6486462,"first_name":"Patrick","middle_initials":null,"last_name":"Redmond","page_name":"RedmondPatrick","domain_name":"independent","created_at":"2013-10-30T07:36:46.107-07:00","display_name":"Patrick Redmond","url":"https://independent.academia.edu/RedmondPatrick"},"attachments":[{"id":49545374,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/49545374/thumbnails/1.jpg","file_name":"gsecongeo.105.1.4320161012-11940-nyt2kg.pdf","download_url":"https://www.academia.edu/attachments/49545374/download_file?st=MTczMjgzMzQzOCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"The_Bingham_Canyon_Porphyry_Cu_Mo_Au_Dep.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/49545374/gsecongeo.105.1.4320161012-11940-nyt2kg-libre.pdf?1476275298=\u0026response-content-disposition=attachment%3B+filename%3DThe_Bingham_Canyon_Porphyry_Cu_Mo_Au_Dep.pdf\u0026Expires=1732837038\u0026Signature=OVHd2cJ4i00LqE~4E9RDXzvHouqVXm8ecT8G4THxdvqJavpUFH9GMk7LaUJvxSLQnASwlnliqYo48mm~Z99STm6RsHcxPX7L93Jc9ZG--YKD0MQPBjURX5pr-0PvfpjAcioCexuIdusvL3ysVWz40IVnsXAwhnr~pDcmY5PUlVEpR1brM7kQfVbMDLVhWR7qqHDhecxwKml0VMagqBWZAYg-51vu2dVHD4UEMzdKLFb3DJf3EIbV2iIHfyV0cDoXgSo6Uh83um70FchJkPrPo-SfwLMk~mqmg8YctFe6jMC-PqKQXnFvWwWeZcyY-K5WazNe3pSRg4HBedtpx~BUoQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":407,"name":"Geochemistry","url":"https://www.academia.edu/Documents/in/Geochemistry"},{"id":2406,"name":"Economic Geology","url":"https://www.academia.edu/Documents/in/Economic_Geology"}],"urls":[{"id":1836446,"url":"http://econgeol.geoscienceworld.org/cgi/doi/10.2113/gsecongeo.105.1.43"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="4938002"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/4938002/Copper_deposition_during_quartz_dissolution_by_cooling_magmatic_hydrothermal_fluids_The_Bingham_porphyry"><img alt="Research paper thumbnail of Copper deposition during quartz dissolution by cooling magmatic hydrothermal fluids: The Bingham porphyry" class="work-thumbnail" src="https://attachments.academia-assets.com/49545299/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/4938002/Copper_deposition_during_quartz_dissolution_by_cooling_magmatic_hydrothermal_fluids_The_Bingham_porphyry">Copper deposition during quartz dissolution by cooling magmatic hydrothermal fluids: The Bingham porphyry</a></div><div class="wp-workCard_item"><span>Earth and Planetary Science Letters</span><span>, 2005</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Scanning electron microscope cathodoluminescence imaging is used to map successive generations of...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Scanning electron microscope cathodoluminescence imaging is used to map successive generations of fluid inclusions in texturally complex quartz veinlets representing the main stage of ore metal introduction into the porphyry Cu-Au-Mo deposit at Bingham, Utah. Following conventional fluid inclusion microthermometry, laser ablation-inductively coupled plasma-mass spectrometry (LA-ICPMS) is applied to quantify copper and other major and trace-element concentrations in the evolving fluid, with the aim of identifying the ore-forming processes. Textures visible in cathodoluminescence consistently show that the bulk of vein quartz (Q1), characterized by bright luminescence, crystallized early in the vein history. Cu-Fe-sulfides are precipitated later in these veins, in a microfracture network finally filled with a second generation of dull-luminescing Q2 quartz. Mapping of brine and vapor inclusion assemblages in these successive quartz generations in combination with LA-ICPMS microanalysis shows that the fluids trapped before and after Cu-Fe-sulfide precipitation are very similar with respect to their major and minor-element composition, except for copper. Copper concentrations in inclusions associated with ore formation drop by two orders of magnitude, in a tight pressure-temperature interval between 21 and 14 MPa and 425-350 °C, several hundred degrees below the temperature of fluid exsolution from the magma. Copper deposition occurs within a limited P- T region, in which sulfide solubility shows strong normal temperature dependence while quartz solubility is retrograde. This permits copper sulfide deposition while secondary vein permeability is generated by quartz dissolution. The brittle-to-ductile transition of the quartz-feldspar-rich host rocks occurs in the same temperature range, which further enhances vein reactivation and promotes cooling and expansion of fluids ascending across the transition from lithostatic to hydrostatic conditions.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="d476edbbc708b99d9311e4d6c25bc4cb" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":49545299,"asset_id":4938002,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/49545299/download_file?st=MTczMjgzMzQzOCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="4938002"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="4938002"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 4938002; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=4938002]").text(description); $(".js-view-count[data-work-id=4938002]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 4938002; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='4938002']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 4938002, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "d476edbbc708b99d9311e4d6c25bc4cb" } } $('.js-work-strip[data-work-id=4938002]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":4938002,"title":"Copper deposition during quartz dissolution by cooling magmatic hydrothermal fluids: The Bingham porphyry","translated_title":"","metadata":{"abstract":"Scanning electron microscope cathodoluminescence imaging is used to map successive generations of fluid inclusions in texturally complex quartz veinlets representing the main stage of ore metal introduction into the porphyry Cu-Au-Mo deposit at Bingham, Utah. Following conventional fluid inclusion microthermometry, laser ablation-inductively coupled plasma-mass spectrometry (LA-ICPMS) is applied to quantify copper and other major and trace-element concentrations in the evolving fluid, with the aim of identifying the ore-forming processes. Textures visible in cathodoluminescence consistently show that the bulk of vein quartz (Q1), characterized by bright luminescence, crystallized early in the vein history. Cu-Fe-sulfides are precipitated later in these veins, in a microfracture network finally filled with a second generation of dull-luminescing Q2 quartz. Mapping of brine and vapor inclusion assemblages in these successive quartz generations in combination with LA-ICPMS microanalysis shows that the fluids trapped before and after Cu-Fe-sulfide precipitation are very similar with respect to their major and minor-element composition, except for copper. Copper concentrations in inclusions associated with ore formation drop by two orders of magnitude, in a tight pressure-temperature interval between 21 and 14 MPa and 425-350 °C, several hundred degrees below the temperature of fluid exsolution from the magma. Copper deposition occurs within a limited P- T region, in which sulfide solubility shows strong normal temperature dependence while quartz solubility is retrograde. This permits copper sulfide deposition while secondary vein permeability is generated by quartz dissolution. The brittle-to-ductile transition of the quartz-feldspar-rich host rocks occurs in the same temperature range, which further enhances vein reactivation and promotes cooling and expansion of fluids ascending across the transition from lithostatic to hydrostatic conditions.","publication_date":{"day":null,"month":null,"year":2005,"errors":{}},"publication_name":"Earth and Planetary Science Letters"},"translated_abstract":"Scanning electron microscope cathodoluminescence imaging is used to map successive generations of fluid inclusions in texturally complex quartz veinlets representing the main stage of ore metal introduction into the porphyry Cu-Au-Mo deposit at Bingham, Utah. Following conventional fluid inclusion microthermometry, laser ablation-inductively coupled plasma-mass spectrometry (LA-ICPMS) is applied to quantify copper and other major and trace-element concentrations in the evolving fluid, with the aim of identifying the ore-forming processes. Textures visible in cathodoluminescence consistently show that the bulk of vein quartz (Q1), characterized by bright luminescence, crystallized early in the vein history. Cu-Fe-sulfides are precipitated later in these veins, in a microfracture network finally filled with a second generation of dull-luminescing Q2 quartz. Mapping of brine and vapor inclusion assemblages in these successive quartz generations in combination with LA-ICPMS microanalysis shows that the fluids trapped before and after Cu-Fe-sulfide precipitation are very similar with respect to their major and minor-element composition, except for copper. Copper concentrations in inclusions associated with ore formation drop by two orders of magnitude, in a tight pressure-temperature interval between 21 and 14 MPa and 425-350 °C, several hundred degrees below the temperature of fluid exsolution from the magma. Copper deposition occurs within a limited P- T region, in which sulfide solubility shows strong normal temperature dependence while quartz solubility is retrograde. This permits copper sulfide deposition while secondary vein permeability is generated by quartz dissolution. The brittle-to-ductile transition of the quartz-feldspar-rich host rocks occurs in the same temperature range, which further enhances vein reactivation and promotes cooling and expansion of fluids ascending across the transition from lithostatic to hydrostatic conditions.","internal_url":"https://www.academia.edu/4938002/Copper_deposition_during_quartz_dissolution_by_cooling_magmatic_hydrothermal_fluids_The_Bingham_porphyry","translated_internal_url":"","created_at":"2013-10-30T07:37:55.793-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":6486462,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":49545299,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/49545299/thumbnails/1.jpg","file_name":"Copper_deposition_during_quartz_dissolut20161012-14633-1wydzju.pdf","download_url":"https://www.academia.edu/attachments/49545299/download_file?st=MTczMjgzMzQzOCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Copper_deposition_during_quartz_dissolut.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/49545299/Copper_deposition_during_quartz_dissolut20161012-14633-1wydzju-libre.pdf?1476275311=\u0026response-content-disposition=attachment%3B+filename%3DCopper_deposition_during_quartz_dissolut.pdf\u0026Expires=1732837038\u0026Signature=YLE6jHBRxrlk0B4NUP4RSfDKbZvKIFE8s9bXeHx6Hgki8VJS8e5PzuGyvA0NiY3fgDQnMnjivhEnVEmmk8M5ltSA1k7LGr5RcuEKf8dtKhMBJ1U-y3vy2R0N1S44YqyZRep23KRqd6W9DKjubzMPfsStkTxbW9lff~r-ZJQ6BNiMTA-qlhIS9uYsbLxOUDT6ruSZR1vEk6NogeWKFrzL6rUTHFlzwlxJXloYTfuCvlG6AH1eSO0OZVBhPYI1OVNdY4wg~XzWM9Mg27xyVw43uccZh5S5VsgD0e0u2LvX4~-RLHq6xAl0N3cOrFMS09-x6VfnjFOgzsXDkVO28XWpTg__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Copper_deposition_during_quartz_dissolution_by_cooling_magmatic_hydrothermal_fluids_The_Bingham_porphyry","translated_slug":"","page_count":15,"language":"en","content_type":"Work","owner":{"id":6486462,"first_name":"Patrick","middle_initials":null,"last_name":"Redmond","page_name":"RedmondPatrick","domain_name":"independent","created_at":"2013-10-30T07:36:46.107-07:00","display_name":"Patrick Redmond","url":"https://independent.academia.edu/RedmondPatrick"},"attachments":[{"id":49545299,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/49545299/thumbnails/1.jpg","file_name":"Copper_deposition_during_quartz_dissolut20161012-14633-1wydzju.pdf","download_url":"https://www.academia.edu/attachments/49545299/download_file?st=MTczMjgzMzQzOCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Copper_deposition_during_quartz_dissolut.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/49545299/Copper_deposition_during_quartz_dissolut20161012-14633-1wydzju-libre.pdf?1476275311=\u0026response-content-disposition=attachment%3B+filename%3DCopper_deposition_during_quartz_dissolut.pdf\u0026Expires=1732837038\u0026Signature=YLE6jHBRxrlk0B4NUP4RSfDKbZvKIFE8s9bXeHx6Hgki8VJS8e5PzuGyvA0NiY3fgDQnMnjivhEnVEmmk8M5ltSA1k7LGr5RcuEKf8dtKhMBJ1U-y3vy2R0N1S44YqyZRep23KRqd6W9DKjubzMPfsStkTxbW9lff~r-ZJQ6BNiMTA-qlhIS9uYsbLxOUDT6ruSZR1vEk6NogeWKFrzL6rUTHFlzwlxJXloYTfuCvlG6AH1eSO0OZVBhPYI1OVNdY4wg~XzWM9Mg27xyVw43uccZh5S5VsgD0e0u2LvX4~-RLHq6xAl0N3cOrFMS09-x6VfnjFOgzsXDkVO28XWpTg__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences"},{"id":80692,"name":"Copper","url":"https://www.academia.edu/Documents/in/Copper"},{"id":103443,"name":"Cathodoluminescence","url":"https://www.academia.edu/Documents/in/Cathodoluminescence"},{"id":118582,"name":"Physical sciences","url":"https://www.academia.edu/Documents/in/Physical_sciences"},{"id":159153,"name":"Laser Ablation","url":"https://www.academia.edu/Documents/in/Laser_Ablation"},{"id":222413,"name":"Inductively Coupled Plasma Mass Spectrometry","url":"https://www.academia.edu/Documents/in/Inductively_Coupled_Plasma_Mass_Spectrometry"},{"id":241723,"name":"Earth and Planetary Science","url":"https://www.academia.edu/Documents/in/Earth_and_Planetary_Science"},{"id":247487,"name":"Temperature Dependence","url":"https://www.academia.edu/Documents/in/Temperature_Dependence"},{"id":390995,"name":"Scanning Electron Microscope","url":"https://www.academia.edu/Documents/in/Scanning_Electron_Microscope"},{"id":527989,"name":"Fluid Inclusion","url":"https://www.academia.edu/Documents/in/Fluid_Inclusion"},{"id":675513,"name":"Earth and Planetary Sciences","url":"https://www.academia.edu/Documents/in/Earth_and_Planetary_Sciences"},{"id":709300,"name":"Trace element","url":"https://www.academia.edu/Documents/in/Trace_element"},{"id":1153440,"name":"Strong Normalization","url":"https://www.academia.edu/Documents/in/Strong_Normalization"}],"urls":[{"id":1836445,"url":"http://adsabs.harvard.edu/abs/2005E\u0026PSL.235..229L"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="4938001"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/4938001/The_Bingham_Canyon_Porphyry_Cu_Mo_Au_Deposit_III_Zoned_Copper_Gold_Ore_Deposition_by_Magmatic_Vapor_Expansion"><img alt="Research paper thumbnail of The Bingham Canyon Porphyry Cu-Mo-Au Deposit. III. Zoned Copper-Gold Ore Deposition by Magmatic Vapor Expansion" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/4938001/The_Bingham_Canyon_Porphyry_Cu_Mo_Au_Deposit_III_Zoned_Copper_Gold_Ore_Deposition_by_Magmatic_Vapor_Expansion">The Bingham Canyon Porphyry Cu-Mo-Au Deposit. III. Zoned Copper-Gold Ore Deposition by Magmatic Vapor Expansion</a></div><div class="wp-workCard_item"><span>Economic Geology</span><span>, 2010</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">ABSTRACT Fluid inclusion microthermometry and laser-ablation ICPMS microanalysis are combined wit...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">ABSTRACT Fluid inclusion microthermometry and laser-ablation ICPMS microanalysis are combined with geological and textural observations to reconstruct the spatial and temporal evolution of magmatic fluids that formed the subvolcanic porphyry Cu-Au(-Mo) ore deposit at Bingham Canyon, Utah. The Bingham Canyon orebody is exposed over similar to 1.6 km vertically and has the shape of to inverted cop with distinct metal zoning. Fluid inclusions in the barren but highly veined and potassically altered deep center of the system have intermediate density (similar to 0.6 g cm(-3)) and a salinity of similar to 7 wt percent NaCl equiv. They have subequal concentrations of Na, K, Fe, Cu and contain minor CO(2). The intermediate-density fluids were trapped as a single phase, mostly at &amp;gt;500 degrees C and &amp;gt;800 bars. The Au-Cu-rich center near the top of the orebody contains low-density vapor inclusions (similar to 0.2 g cm(-3)) coexisting with brine inclusions containing similar to 45 wt. percent NaCl equiv. The vertical transition Of different inclusion types indicates phase separation of the single-phase input fluid upon volume expansion associated with a pressure drop to 200 +/- 100 liars. Mass-balance calculation based on all analyzed inclusion components indicates that the mass of the vapor phase exceeded that of the brine by similar to 9/1. The vapor contained Cu as its dominant cation (similar to 1.5 wt%) and contributed about 9.5 percent of the total amount of copper transported to the base of the orebody. Bornite. chalcopyrite, and native gold were precipitated in a narrow temperature interval from 430 degrees to 350 degrees C, into secondary pore space created by local redissolution of vein quartz as a result id quartz solubility in the vapor-dominated fluid system. Intermediate-density fluid inclusions in the deepest parts of the peripheral copper ore zone have identical density and composition, including similar gold contents, as those in the deep center. Microthermometry and statistical estimation of phase proportions in the inclusions show that the vapor in the peripheral Cu-rich but Au-poor ore zone remained denser, and the separating brine was less saline (similar to 36 wt% NaCl equiv), compared to vapor and brine in the central Au-Cu ore zone. This indicates that the peripheral fluids experienced a lower degree of phase separation, due to slightly higher fluid pressure at equivalent temperature, compared to more strongly expanding fluids in the center oldie system. The systematic zoning or Au/Cu within the ore shell, despite compositionally similar input Hinds. is interpreted to have resulted from slightly different pressure-temperature-density evolution paths of magmatic fluids. Copper was selectively precipitated in the peripheral ore zone, in contrast to complete coprecipitation of Au and Cu ill the central upflow zone of the vapor plume. The formation of particularly rich Cu-Au ore in the center of the upward-expanding fluid plume is consistent with published experimental data, showing that the solubility metals in hydrous vapor decreases sharply with falling pressure. due to destabilization of the hydration shell around metal complexes in expanding vapor. This interpretation supports the classic vapor plume model for porphyry clipper ore formation but additionally emphasizes the role of sulfur-bearing complexes as a key chemical control on magmatic-hydrothermal Metal transport and the deposition of Cu and Au in porphyry ores. Our interpretation of selective Cu +/- Au precipitation as a function of vapor density can explain die more general observation that most gold-rich porphyry copper deposits;tie formed in shallow sub-volcanic environments. whereas deeper scated porphyry Cu-(Mo) deposits are generally gold poor.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="4938001"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="4938001"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 4938001; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=4938001]").text(description); $(".js-view-count[data-work-id=4938001]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 4938001; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='4938001']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 4938001, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=4938001]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":4938001,"title":"The Bingham Canyon Porphyry Cu-Mo-Au Deposit. III. Zoned Copper-Gold Ore Deposition by Magmatic Vapor Expansion","translated_title":"","metadata":{"abstract":"ABSTRACT Fluid inclusion microthermometry and laser-ablation ICPMS microanalysis are combined with geological and textural observations to reconstruct the spatial and temporal evolution of magmatic fluids that formed the subvolcanic porphyry Cu-Au(-Mo) ore deposit at Bingham Canyon, Utah. The Bingham Canyon orebody is exposed over similar to 1.6 km vertically and has the shape of to inverted cop with distinct metal zoning. Fluid inclusions in the barren but highly veined and potassically altered deep center of the system have intermediate density (similar to 0.6 g cm(-3)) and a salinity of similar to 7 wt percent NaCl equiv. They have subequal concentrations of Na, K, Fe, Cu and contain minor CO(2). The intermediate-density fluids were trapped as a single phase, mostly at \u0026amp;gt;500 degrees C and \u0026amp;gt;800 bars. The Au-Cu-rich center near the top of the orebody contains low-density vapor inclusions (similar to 0.2 g cm(-3)) coexisting with brine inclusions containing similar to 45 wt. percent NaCl equiv. The vertical transition Of different inclusion types indicates phase separation of the single-phase input fluid upon volume expansion associated with a pressure drop to 200 +/- 100 liars. Mass-balance calculation based on all analyzed inclusion components indicates that the mass of the vapor phase exceeded that of the brine by similar to 9/1. The vapor contained Cu as its dominant cation (similar to 1.5 wt%) and contributed about 9.5 percent of the total amount of copper transported to the base of the orebody. Bornite. chalcopyrite, and native gold were precipitated in a narrow temperature interval from 430 degrees to 350 degrees C, into secondary pore space created by local redissolution of vein quartz as a result id quartz solubility in the vapor-dominated fluid system. Intermediate-density fluid inclusions in the deepest parts of the peripheral copper ore zone have identical density and composition, including similar gold contents, as those in the deep center. Microthermometry and statistical estimation of phase proportions in the inclusions show that the vapor in the peripheral Cu-rich but Au-poor ore zone remained denser, and the separating brine was less saline (similar to 36 wt% NaCl equiv), compared to vapor and brine in the central Au-Cu ore zone. This indicates that the peripheral fluids experienced a lower degree of phase separation, due to slightly higher fluid pressure at equivalent temperature, compared to more strongly expanding fluids in the center oldie system. The systematic zoning or Au/Cu within the ore shell, despite compositionally similar input Hinds. is interpreted to have resulted from slightly different pressure-temperature-density evolution paths of magmatic fluids. Copper was selectively precipitated in the peripheral ore zone, in contrast to complete coprecipitation of Au and Cu ill the central upflow zone of the vapor plume. The formation of particularly rich Cu-Au ore in the center of the upward-expanding fluid plume is consistent with published experimental data, showing that the solubility metals in hydrous vapor decreases sharply with falling pressure. due to destabilization of the hydration shell around metal complexes in expanding vapor. This interpretation supports the classic vapor plume model for porphyry clipper ore formation but additionally emphasizes the role of sulfur-bearing complexes as a key chemical control on magmatic-hydrothermal Metal transport and the deposition of Cu and Au in porphyry ores. Our interpretation of selective Cu +/- Au precipitation as a function of vapor density can explain die more general observation that most gold-rich porphyry copper deposits;tie formed in shallow sub-volcanic environments. whereas deeper scated porphyry Cu-(Mo) deposits are generally gold poor.","publication_date":{"day":null,"month":null,"year":2010,"errors":{}},"publication_name":"Economic Geology"},"translated_abstract":"ABSTRACT Fluid inclusion microthermometry and laser-ablation ICPMS microanalysis are combined with geological and textural observations to reconstruct the spatial and temporal evolution of magmatic fluids that formed the subvolcanic porphyry Cu-Au(-Mo) ore deposit at Bingham Canyon, Utah. The Bingham Canyon orebody is exposed over similar to 1.6 km vertically and has the shape of to inverted cop with distinct metal zoning. Fluid inclusions in the barren but highly veined and potassically altered deep center of the system have intermediate density (similar to 0.6 g cm(-3)) and a salinity of similar to 7 wt percent NaCl equiv. They have subequal concentrations of Na, K, Fe, Cu and contain minor CO(2). The intermediate-density fluids were trapped as a single phase, mostly at \u0026amp;gt;500 degrees C and \u0026amp;gt;800 bars. The Au-Cu-rich center near the top of the orebody contains low-density vapor inclusions (similar to 0.2 g cm(-3)) coexisting with brine inclusions containing similar to 45 wt. percent NaCl equiv. The vertical transition Of different inclusion types indicates phase separation of the single-phase input fluid upon volume expansion associated with a pressure drop to 200 +/- 100 liars. Mass-balance calculation based on all analyzed inclusion components indicates that the mass of the vapor phase exceeded that of the brine by similar to 9/1. The vapor contained Cu as its dominant cation (similar to 1.5 wt%) and contributed about 9.5 percent of the total amount of copper transported to the base of the orebody. Bornite. chalcopyrite, and native gold were precipitated in a narrow temperature interval from 430 degrees to 350 degrees C, into secondary pore space created by local redissolution of vein quartz as a result id quartz solubility in the vapor-dominated fluid system. Intermediate-density fluid inclusions in the deepest parts of the peripheral copper ore zone have identical density and composition, including similar gold contents, as those in the deep center. Microthermometry and statistical estimation of phase proportions in the inclusions show that the vapor in the peripheral Cu-rich but Au-poor ore zone remained denser, and the separating brine was less saline (similar to 36 wt% NaCl equiv), compared to vapor and brine in the central Au-Cu ore zone. This indicates that the peripheral fluids experienced a lower degree of phase separation, due to slightly higher fluid pressure at equivalent temperature, compared to more strongly expanding fluids in the center oldie system. The systematic zoning or Au/Cu within the ore shell, despite compositionally similar input Hinds. is interpreted to have resulted from slightly different pressure-temperature-density evolution paths of magmatic fluids. Copper was selectively precipitated in the peripheral ore zone, in contrast to complete coprecipitation of Au and Cu ill the central upflow zone of the vapor plume. The formation of particularly rich Cu-Au ore in the center of the upward-expanding fluid plume is consistent with published experimental data, showing that the solubility metals in hydrous vapor decreases sharply with falling pressure. due to destabilization of the hydration shell around metal complexes in expanding vapor. This interpretation supports the classic vapor plume model for porphyry clipper ore formation but additionally emphasizes the role of sulfur-bearing complexes as a key chemical control on magmatic-hydrothermal Metal transport and the deposition of Cu and Au in porphyry ores. 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Qualitative analysis of interview data and curriculum documentation collected from the schools provide a model of the curriculum process which is firmly grounded in the data. Comparisons across the categories of the model indicate strong differences between the schools</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="4938000"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="4938000"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 4938000; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=4938000]").text(description); $(".js-view-count[data-work-id=4938000]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 4938000; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='4938000']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 4938000, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=4938000]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":4938000,"title":"Comparing the curriculum development process in special (MLD) schools: a systematic qualitative approach","translated_title":"","metadata":{"abstract":"The present paper describes a comparative study of ten special schools for pupils with moderate learning difficulties in England and Wales. 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> </div><div class="profile--tab_content_container js-tab-pane tab-pane" data-section-id="857145" id="papers"><div class="js-work-strip profile--work_container" data-work-id="4938012"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/4938012/Closure_to_Solute_Breakthrough_Curves_for_Processed_Kaolin_at_Low_Flow_Rates_by_Charles_D_Shackelford_and_Patrick_L_Redmond"><img alt="Research paper thumbnail of Closure to “Solute Breakthrough Curves for Processed Kaolin at Low Flow Rates” by Charles D. 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Redmond</a></div><div class="wp-workCard_item"><span>Journal of Geotechnical Engineering</span><span>, 1996</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="81f0c055ffe31fc903341bee13b7e38b" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":49545275,"asset_id":4938012,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/49545275/download_file?st=MTczMjgzMzQzOSw4LjIyMi4yMDguMTQ2&st=MTczMjgzMzQzOCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="4938012"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="4938012"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 4938012; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=4938012]").text(description); $(".js-view-count[data-work-id=4938012]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 4938012; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='4938012']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 4938012, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "81f0c055ffe31fc903341bee13b7e38b" } } $('.js-work-strip[data-work-id=4938012]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":4938012,"title":"Closure to “Solute Breakthrough Curves for Processed Kaolin at Low Flow Rates” by Charles D. 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Unlike verification, validation is typically an ill-defined activity for software development. This paper presents a well-defined validation metrics framework which uses hazard analysis, and the derived software requirements for mitigating the identified hazards, as proxies in gauging the sufficiency of the software safety requirements early in the software development process. Moreover, traditional hazard analysis techniques are insufficient to deal with the complexity and size of systems of systems. 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href="https://www.academia.edu/4938006/Interface_hazard_analysis_for_system_of_systems"><img alt="Research paper thumbnail of Interface hazard analysis for system of systems" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/4938006/Interface_hazard_analysis_for_system_of_systems">Interface hazard analysis for system of systems</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The next generation of military capabilities will hinge on systems of systems. Such systems can i...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The next generation of military capabilities will hinge on systems of systems. Such systems can introduce emergent hazards that must be adequately dealt with before the system of systems can be employed. Traditional hazard analysis techniques do not address the complexity and size of systems of systems. In this paper we describe a technique for conducting interface hazard analysis for systems of systems. The technique is compatible with current system safety processes.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="4938006"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="4938006"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 4938006; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=4938006]").text(description); $(".js-view-count[data-work-id=4938006]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 4938006; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='4938006']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 4938006, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=4938006]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":4938006,"title":"Interface hazard analysis for system of systems","translated_title":"","metadata":{"abstract":"The next generation of military capabilities will hinge on systems of systems. 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At Bingham, we see no change in the style of wall-rock alteration associated with the ... C, ...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">... At Bingham, we see no change in the style of wall-rock alteration associated with the ... C, during the late Q2 quartz deposition in equilibrium with K-feldspar + biotite, was the ... of an intrusion-centered hydrothermal system: Far SoutheastLepanto porphyry and epithermal Cu-...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="4938005"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="4938005"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 4938005; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=4938005]").text(description); $(".js-view-count[data-work-id=4938005]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 4938005; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='4938005']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 4938005, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=4938005]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":4938005,"title":"Copper deposition by fluid cooling in intrusion-centered systems: New insights from the Bingham porphyry ore deposit, Utah","translated_title":"","metadata":{"abstract":"... 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I. Sequence of Intrusions, Vein Formation, and Sulfide Deposition" class="work-thumbnail" src="https://attachments.academia-assets.com/49545374/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/4938003/The_Bingham_Canyon_Porphyry_Cu_Mo_Au_Deposit_I_Sequence_of_Intrusions_Vein_Formation_and_Sulfide_Deposition">The Bingham Canyon Porphyry Cu-Mo-Au Deposit. I. Sequence of Intrusions, Vein Formation, and Sulfide Deposition</a></div><div class="wp-workCard_item"><span>Economic Geology</span><span>, 2010</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="ec644ccecddc645af1f62db92fd390f8" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":49545374,"asset_id":4938003,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/49545374/download_file?st=MTczMjgzMzQzOSw4LjIyMi4yMDguMTQ2&st=MTczMjgzMzQzOCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="4938003"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="4938003"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 4938003; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=4938003]").text(description); $(".js-view-count[data-work-id=4938003]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 4938003; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='4938003']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 4938003, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "ec644ccecddc645af1f62db92fd390f8" } } $('.js-work-strip[data-work-id=4938003]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":4938003,"title":"The Bingham Canyon Porphyry Cu-Mo-Au Deposit. I. Sequence of Intrusions, Vein Formation, and Sulfide Deposition","translated_title":"","metadata":{"grobid_abstract":"The Bingham Canyon porphyry copper-gold-molybdenum deposit is one of the largest and highest-grade porphyry orebodies in the world. This study focused on the northwest side of the deposit where quartz monzonite porphyry (QMP), the first and largest porphyry intrusion, hosts the bulk of the high-grade copper-gold ore (\u003e1.0% Cu, \u003e1.0 ppm Au). The north-northeast-trending, high-grade zone had pre-mining dimensions of 1,500 m strike, \u003e300 m vertical, and 500 m width and contained more than 500 million tonnes (Mt) of ore associated with potassic alteration and abundant quartz veins. The lack of superimposed sericitic alteration yielded ideal exposures in which to study the early, high-temperature stages of ore formation, a style of mineralization that in many porphyry deposits represents the major period of copper introduction.","publication_date":{"day":null,"month":null,"year":2010,"errors":{}},"publication_name":"Economic Geology","grobid_abstract_attachment_id":49545374},"translated_abstract":null,"internal_url":"https://www.academia.edu/4938003/The_Bingham_Canyon_Porphyry_Cu_Mo_Au_Deposit_I_Sequence_of_Intrusions_Vein_Formation_and_Sulfide_Deposition","translated_internal_url":"","created_at":"2013-10-30T07:37:56.283-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":6486462,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":49545374,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/49545374/thumbnails/1.jpg","file_name":"gsecongeo.105.1.4320161012-11940-nyt2kg.pdf","download_url":"https://www.academia.edu/attachments/49545374/download_file?st=MTczMjgzMzQzOSw4LjIyMi4yMDguMTQ2&st=MTczMjgzMzQzOCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"The_Bingham_Canyon_Porphyry_Cu_Mo_Au_Dep.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/49545374/gsecongeo.105.1.4320161012-11940-nyt2kg-libre.pdf?1476275298=\u0026response-content-disposition=attachment%3B+filename%3DThe_Bingham_Canyon_Porphyry_Cu_Mo_Au_Dep.pdf\u0026Expires=1732837038\u0026Signature=OVHd2cJ4i00LqE~4E9RDXzvHouqVXm8ecT8G4THxdvqJavpUFH9GMk7LaUJvxSLQnASwlnliqYo48mm~Z99STm6RsHcxPX7L93Jc9ZG--YKD0MQPBjURX5pr-0PvfpjAcioCexuIdusvL3ysVWz40IVnsXAwhnr~pDcmY5PUlVEpR1brM7kQfVbMDLVhWR7qqHDhecxwKml0VMagqBWZAYg-51vu2dVHD4UEMzdKLFb3DJf3EIbV2iIHfyV0cDoXgSo6Uh83um70FchJkPrPo-SfwLMk~mqmg8YctFe6jMC-PqKQXnFvWwWeZcyY-K5WazNe3pSRg4HBedtpx~BUoQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"The_Bingham_Canyon_Porphyry_Cu_Mo_Au_Deposit_I_Sequence_of_Intrusions_Vein_Formation_and_Sulfide_Deposition","translated_slug":"","page_count":26,"language":"en","content_type":"Work","owner":{"id":6486462,"first_name":"Patrick","middle_initials":null,"last_name":"Redmond","page_name":"RedmondPatrick","domain_name":"independent","created_at":"2013-10-30T07:36:46.107-07:00","display_name":"Patrick Redmond","url":"https://independent.academia.edu/RedmondPatrick"},"attachments":[{"id":49545374,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/49545374/thumbnails/1.jpg","file_name":"gsecongeo.105.1.4320161012-11940-nyt2kg.pdf","download_url":"https://www.academia.edu/attachments/49545374/download_file?st=MTczMjgzMzQzOSw4LjIyMi4yMDguMTQ2&st=MTczMjgzMzQzOCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"The_Bingham_Canyon_Porphyry_Cu_Mo_Au_Dep.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/49545374/gsecongeo.105.1.4320161012-11940-nyt2kg-libre.pdf?1476275298=\u0026response-content-disposition=attachment%3B+filename%3DThe_Bingham_Canyon_Porphyry_Cu_Mo_Au_Dep.pdf\u0026Expires=1732837038\u0026Signature=OVHd2cJ4i00LqE~4E9RDXzvHouqVXm8ecT8G4THxdvqJavpUFH9GMk7LaUJvxSLQnASwlnliqYo48mm~Z99STm6RsHcxPX7L93Jc9ZG--YKD0MQPBjURX5pr-0PvfpjAcioCexuIdusvL3ysVWz40IVnsXAwhnr~pDcmY5PUlVEpR1brM7kQfVbMDLVhWR7qqHDhecxwKml0VMagqBWZAYg-51vu2dVHD4UEMzdKLFb3DJf3EIbV2iIHfyV0cDoXgSo6Uh83um70FchJkPrPo-SfwLMk~mqmg8YctFe6jMC-PqKQXnFvWwWeZcyY-K5WazNe3pSRg4HBedtpx~BUoQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":407,"name":"Geochemistry","url":"https://www.academia.edu/Documents/in/Geochemistry"},{"id":2406,"name":"Economic Geology","url":"https://www.academia.edu/Documents/in/Economic_Geology"}],"urls":[{"id":1836446,"url":"http://econgeol.geoscienceworld.org/cgi/doi/10.2113/gsecongeo.105.1.43"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="4938002"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/4938002/Copper_deposition_during_quartz_dissolution_by_cooling_magmatic_hydrothermal_fluids_The_Bingham_porphyry"><img alt="Research paper thumbnail of Copper deposition during quartz dissolution by cooling magmatic hydrothermal fluids: The Bingham porphyry" class="work-thumbnail" src="https://attachments.academia-assets.com/49545299/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/4938002/Copper_deposition_during_quartz_dissolution_by_cooling_magmatic_hydrothermal_fluids_The_Bingham_porphyry">Copper deposition during quartz dissolution by cooling magmatic hydrothermal fluids: The Bingham porphyry</a></div><div class="wp-workCard_item"><span>Earth and Planetary Science Letters</span><span>, 2005</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Scanning electron microscope cathodoluminescence imaging is used to map successive generations of...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Scanning electron microscope cathodoluminescence imaging is used to map successive generations of fluid inclusions in texturally complex quartz veinlets representing the main stage of ore metal introduction into the porphyry Cu-Au-Mo deposit at Bingham, Utah. Following conventional fluid inclusion microthermometry, laser ablation-inductively coupled plasma-mass spectrometry (LA-ICPMS) is applied to quantify copper and other major and trace-element concentrations in the evolving fluid, with the aim of identifying the ore-forming processes. Textures visible in cathodoluminescence consistently show that the bulk of vein quartz (Q1), characterized by bright luminescence, crystallized early in the vein history. Cu-Fe-sulfides are precipitated later in these veins, in a microfracture network finally filled with a second generation of dull-luminescing Q2 quartz. Mapping of brine and vapor inclusion assemblages in these successive quartz generations in combination with LA-ICPMS microanalysis shows that the fluids trapped before and after Cu-Fe-sulfide precipitation are very similar with respect to their major and minor-element composition, except for copper. Copper concentrations in inclusions associated with ore formation drop by two orders of magnitude, in a tight pressure-temperature interval between 21 and 14 MPa and 425-350 °C, several hundred degrees below the temperature of fluid exsolution from the magma. Copper deposition occurs within a limited P- T region, in which sulfide solubility shows strong normal temperature dependence while quartz solubility is retrograde. This permits copper sulfide deposition while secondary vein permeability is generated by quartz dissolution. The brittle-to-ductile transition of the quartz-feldspar-rich host rocks occurs in the same temperature range, which further enhances vein reactivation and promotes cooling and expansion of fluids ascending across the transition from lithostatic to hydrostatic conditions.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="d476edbbc708b99d9311e4d6c25bc4cb" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":49545299,"asset_id":4938002,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/49545299/download_file?st=MTczMjgzMzQzOSw4LjIyMi4yMDguMTQ2&st=MTczMjgzMzQzOCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="4938002"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="4938002"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 4938002; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=4938002]").text(description); $(".js-view-count[data-work-id=4938002]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 4938002; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='4938002']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 4938002, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "d476edbbc708b99d9311e4d6c25bc4cb" } } $('.js-work-strip[data-work-id=4938002]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":4938002,"title":"Copper deposition during quartz dissolution by cooling magmatic hydrothermal fluids: The Bingham porphyry","translated_title":"","metadata":{"abstract":"Scanning electron microscope cathodoluminescence imaging is used to map successive generations of fluid inclusions in texturally complex quartz veinlets representing the main stage of ore metal introduction into the porphyry Cu-Au-Mo deposit at Bingham, Utah. Following conventional fluid inclusion microthermometry, laser ablation-inductively coupled plasma-mass spectrometry (LA-ICPMS) is applied to quantify copper and other major and trace-element concentrations in the evolving fluid, with the aim of identifying the ore-forming processes. Textures visible in cathodoluminescence consistently show that the bulk of vein quartz (Q1), characterized by bright luminescence, crystallized early in the vein history. Cu-Fe-sulfides are precipitated later in these veins, in a microfracture network finally filled with a second generation of dull-luminescing Q2 quartz. Mapping of brine and vapor inclusion assemblages in these successive quartz generations in combination with LA-ICPMS microanalysis shows that the fluids trapped before and after Cu-Fe-sulfide precipitation are very similar with respect to their major and minor-element composition, except for copper. Copper concentrations in inclusions associated with ore formation drop by two orders of magnitude, in a tight pressure-temperature interval between 21 and 14 MPa and 425-350 °C, several hundred degrees below the temperature of fluid exsolution from the magma. Copper deposition occurs within a limited P- T region, in which sulfide solubility shows strong normal temperature dependence while quartz solubility is retrograde. This permits copper sulfide deposition while secondary vein permeability is generated by quartz dissolution. The brittle-to-ductile transition of the quartz-feldspar-rich host rocks occurs in the same temperature range, which further enhances vein reactivation and promotes cooling and expansion of fluids ascending across the transition from lithostatic to hydrostatic conditions.","publication_date":{"day":null,"month":null,"year":2005,"errors":{}},"publication_name":"Earth and Planetary Science Letters"},"translated_abstract":"Scanning electron microscope cathodoluminescence imaging is used to map successive generations of fluid inclusions in texturally complex quartz veinlets representing the main stage of ore metal introduction into the porphyry Cu-Au-Mo deposit at Bingham, Utah. Following conventional fluid inclusion microthermometry, laser ablation-inductively coupled plasma-mass spectrometry (LA-ICPMS) is applied to quantify copper and other major and trace-element concentrations in the evolving fluid, with the aim of identifying the ore-forming processes. Textures visible in cathodoluminescence consistently show that the bulk of vein quartz (Q1), characterized by bright luminescence, crystallized early in the vein history. Cu-Fe-sulfides are precipitated later in these veins, in a microfracture network finally filled with a second generation of dull-luminescing Q2 quartz. Mapping of brine and vapor inclusion assemblages in these successive quartz generations in combination with LA-ICPMS microanalysis shows that the fluids trapped before and after Cu-Fe-sulfide precipitation are very similar with respect to their major and minor-element composition, except for copper. Copper concentrations in inclusions associated with ore formation drop by two orders of magnitude, in a tight pressure-temperature interval between 21 and 14 MPa and 425-350 °C, several hundred degrees below the temperature of fluid exsolution from the magma. Copper deposition occurs within a limited P- T region, in which sulfide solubility shows strong normal temperature dependence while quartz solubility is retrograde. This permits copper sulfide deposition while secondary vein permeability is generated by quartz dissolution. The brittle-to-ductile transition of the quartz-feldspar-rich host rocks occurs in the same temperature range, which further enhances vein reactivation and promotes cooling and expansion of fluids ascending across the transition from lithostatic to hydrostatic conditions.","internal_url":"https://www.academia.edu/4938002/Copper_deposition_during_quartz_dissolution_by_cooling_magmatic_hydrothermal_fluids_The_Bingham_porphyry","translated_internal_url":"","created_at":"2013-10-30T07:37:55.793-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":6486462,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":49545299,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/49545299/thumbnails/1.jpg","file_name":"Copper_deposition_during_quartz_dissolut20161012-14633-1wydzju.pdf","download_url":"https://www.academia.edu/attachments/49545299/download_file?st=MTczMjgzMzQzOSw4LjIyMi4yMDguMTQ2&st=MTczMjgzMzQzOCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Copper_deposition_during_quartz_dissolut.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/49545299/Copper_deposition_during_quartz_dissolut20161012-14633-1wydzju-libre.pdf?1476275311=\u0026response-content-disposition=attachment%3B+filename%3DCopper_deposition_during_quartz_dissolut.pdf\u0026Expires=1732837038\u0026Signature=YLE6jHBRxrlk0B4NUP4RSfDKbZvKIFE8s9bXeHx6Hgki8VJS8e5PzuGyvA0NiY3fgDQnMnjivhEnVEmmk8M5ltSA1k7LGr5RcuEKf8dtKhMBJ1U-y3vy2R0N1S44YqyZRep23KRqd6W9DKjubzMPfsStkTxbW9lff~r-ZJQ6BNiMTA-qlhIS9uYsbLxOUDT6ruSZR1vEk6NogeWKFrzL6rUTHFlzwlxJXloYTfuCvlG6AH1eSO0OZVBhPYI1OVNdY4wg~XzWM9Mg27xyVw43uccZh5S5VsgD0e0u2LvX4~-RLHq6xAl0N3cOrFMS09-x6VfnjFOgzsXDkVO28XWpTg__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Copper_deposition_during_quartz_dissolution_by_cooling_magmatic_hydrothermal_fluids_The_Bingham_porphyry","translated_slug":"","page_count":15,"language":"en","content_type":"Work","owner":{"id":6486462,"first_name":"Patrick","middle_initials":null,"last_name":"Redmond","page_name":"RedmondPatrick","domain_name":"independent","created_at":"2013-10-30T07:36:46.107-07:00","display_name":"Patrick 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Microscope","url":"https://www.academia.edu/Documents/in/Scanning_Electron_Microscope"},{"id":527989,"name":"Fluid Inclusion","url":"https://www.academia.edu/Documents/in/Fluid_Inclusion"},{"id":675513,"name":"Earth and Planetary Sciences","url":"https://www.academia.edu/Documents/in/Earth_and_Planetary_Sciences"},{"id":709300,"name":"Trace element","url":"https://www.academia.edu/Documents/in/Trace_element"},{"id":1153440,"name":"Strong Normalization","url":"https://www.academia.edu/Documents/in/Strong_Normalization"}],"urls":[{"id":1836445,"url":"http://adsabs.harvard.edu/abs/2005E\u0026PSL.235..229L"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="4938001"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/4938001/The_Bingham_Canyon_Porphyry_Cu_Mo_Au_Deposit_III_Zoned_Copper_Gold_Ore_Deposition_by_Magmatic_Vapor_Expansion"><img alt="Research paper thumbnail of The Bingham Canyon Porphyry Cu-Mo-Au Deposit. III. Zoned Copper-Gold Ore Deposition by Magmatic Vapor Expansion" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/4938001/The_Bingham_Canyon_Porphyry_Cu_Mo_Au_Deposit_III_Zoned_Copper_Gold_Ore_Deposition_by_Magmatic_Vapor_Expansion">The Bingham Canyon Porphyry Cu-Mo-Au Deposit. III. Zoned Copper-Gold Ore Deposition by Magmatic Vapor Expansion</a></div><div class="wp-workCard_item"><span>Economic Geology</span><span>, 2010</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">ABSTRACT Fluid inclusion microthermometry and laser-ablation ICPMS microanalysis are combined wit...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">ABSTRACT Fluid inclusion microthermometry and laser-ablation ICPMS microanalysis are combined with geological and textural observations to reconstruct the spatial and temporal evolution of magmatic fluids that formed the subvolcanic porphyry Cu-Au(-Mo) ore deposit at Bingham Canyon, Utah. The Bingham Canyon orebody is exposed over similar to 1.6 km vertically and has the shape of to inverted cop with distinct metal zoning. Fluid inclusions in the barren but highly veined and potassically altered deep center of the system have intermediate density (similar to 0.6 g cm(-3)) and a salinity of similar to 7 wt percent NaCl equiv. They have subequal concentrations of Na, K, Fe, Cu and contain minor CO(2). The intermediate-density fluids were trapped as a single phase, mostly at &amp;gt;500 degrees C and &amp;gt;800 bars. The Au-Cu-rich center near the top of the orebody contains low-density vapor inclusions (similar to 0.2 g cm(-3)) coexisting with brine inclusions containing similar to 45 wt. percent NaCl equiv. The vertical transition Of different inclusion types indicates phase separation of the single-phase input fluid upon volume expansion associated with a pressure drop to 200 +/- 100 liars. Mass-balance calculation based on all analyzed inclusion components indicates that the mass of the vapor phase exceeded that of the brine by similar to 9/1. The vapor contained Cu as its dominant cation (similar to 1.5 wt%) and contributed about 9.5 percent of the total amount of copper transported to the base of the orebody. Bornite. chalcopyrite, and native gold were precipitated in a narrow temperature interval from 430 degrees to 350 degrees C, into secondary pore space created by local redissolution of vein quartz as a result id quartz solubility in the vapor-dominated fluid system. Intermediate-density fluid inclusions in the deepest parts of the peripheral copper ore zone have identical density and composition, including similar gold contents, as those in the deep center. Microthermometry and statistical estimation of phase proportions in the inclusions show that the vapor in the peripheral Cu-rich but Au-poor ore zone remained denser, and the separating brine was less saline (similar to 36 wt% NaCl equiv), compared to vapor and brine in the central Au-Cu ore zone. This indicates that the peripheral fluids experienced a lower degree of phase separation, due to slightly higher fluid pressure at equivalent temperature, compared to more strongly expanding fluids in the center oldie system. The systematic zoning or Au/Cu within the ore shell, despite compositionally similar input Hinds. is interpreted to have resulted from slightly different pressure-temperature-density evolution paths of magmatic fluids. Copper was selectively precipitated in the peripheral ore zone, in contrast to complete coprecipitation of Au and Cu ill the central upflow zone of the vapor plume. The formation of particularly rich Cu-Au ore in the center of the upward-expanding fluid plume is consistent with published experimental data, showing that the solubility metals in hydrous vapor decreases sharply with falling pressure. due to destabilization of the hydration shell around metal complexes in expanding vapor. This interpretation supports the classic vapor plume model for porphyry clipper ore formation but additionally emphasizes the role of sulfur-bearing complexes as a key chemical control on magmatic-hydrothermal Metal transport and the deposition of Cu and Au in porphyry ores. Our interpretation of selective Cu +/- Au precipitation as a function of vapor density can explain die more general observation that most gold-rich porphyry copper deposits;tie formed in shallow sub-volcanic environments. whereas deeper scated porphyry Cu-(Mo) deposits are generally gold poor.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="4938001"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="4938001"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 4938001; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=4938001]").text(description); $(".js-view-count[data-work-id=4938001]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 4938001; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='4938001']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 4938001, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=4938001]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":4938001,"title":"The Bingham Canyon Porphyry Cu-Mo-Au Deposit. III. Zoned Copper-Gold Ore Deposition by Magmatic Vapor Expansion","translated_title":"","metadata":{"abstract":"ABSTRACT Fluid inclusion microthermometry and laser-ablation ICPMS microanalysis are combined with geological and textural observations to reconstruct the spatial and temporal evolution of magmatic fluids that formed the subvolcanic porphyry Cu-Au(-Mo) ore deposit at Bingham Canyon, Utah. The Bingham Canyon orebody is exposed over similar to 1.6 km vertically and has the shape of to inverted cop with distinct metal zoning. Fluid inclusions in the barren but highly veined and potassically altered deep center of the system have intermediate density (similar to 0.6 g cm(-3)) and a salinity of similar to 7 wt percent NaCl equiv. They have subequal concentrations of Na, K, Fe, Cu and contain minor CO(2). The intermediate-density fluids were trapped as a single phase, mostly at \u0026amp;gt;500 degrees C and \u0026amp;gt;800 bars. The Au-Cu-rich center near the top of the orebody contains low-density vapor inclusions (similar to 0.2 g cm(-3)) coexisting with brine inclusions containing similar to 45 wt. percent NaCl equiv. The vertical transition Of different inclusion types indicates phase separation of the single-phase input fluid upon volume expansion associated with a pressure drop to 200 +/- 100 liars. Mass-balance calculation based on all analyzed inclusion components indicates that the mass of the vapor phase exceeded that of the brine by similar to 9/1. The vapor contained Cu as its dominant cation (similar to 1.5 wt%) and contributed about 9.5 percent of the total amount of copper transported to the base of the orebody. Bornite. chalcopyrite, and native gold were precipitated in a narrow temperature interval from 430 degrees to 350 degrees C, into secondary pore space created by local redissolution of vein quartz as a result id quartz solubility in the vapor-dominated fluid system. Intermediate-density fluid inclusions in the deepest parts of the peripheral copper ore zone have identical density and composition, including similar gold contents, as those in the deep center. Microthermometry and statistical estimation of phase proportions in the inclusions show that the vapor in the peripheral Cu-rich but Au-poor ore zone remained denser, and the separating brine was less saline (similar to 36 wt% NaCl equiv), compared to vapor and brine in the central Au-Cu ore zone. This indicates that the peripheral fluids experienced a lower degree of phase separation, due to slightly higher fluid pressure at equivalent temperature, compared to more strongly expanding fluids in the center oldie system. The systematic zoning or Au/Cu within the ore shell, despite compositionally similar input Hinds. is interpreted to have resulted from slightly different pressure-temperature-density evolution paths of magmatic fluids. Copper was selectively precipitated in the peripheral ore zone, in contrast to complete coprecipitation of Au and Cu ill the central upflow zone of the vapor plume. The formation of particularly rich Cu-Au ore in the center of the upward-expanding fluid plume is consistent with published experimental data, showing that the solubility metals in hydrous vapor decreases sharply with falling pressure. due to destabilization of the hydration shell around metal complexes in expanding vapor. This interpretation supports the classic vapor plume model for porphyry clipper ore formation but additionally emphasizes the role of sulfur-bearing complexes as a key chemical control on magmatic-hydrothermal Metal transport and the deposition of Cu and Au in porphyry ores. Our interpretation of selective Cu +/- Au precipitation as a function of vapor density can explain die more general observation that most gold-rich porphyry copper deposits;tie formed in shallow sub-volcanic environments. whereas deeper scated porphyry Cu-(Mo) deposits are generally gold poor.","publication_date":{"day":null,"month":null,"year":2010,"errors":{}},"publication_name":"Economic Geology"},"translated_abstract":"ABSTRACT Fluid inclusion microthermometry and laser-ablation ICPMS microanalysis are combined with geological and textural observations to reconstruct the spatial and temporal evolution of magmatic fluids that formed the subvolcanic porphyry Cu-Au(-Mo) ore deposit at Bingham Canyon, Utah. The Bingham Canyon orebody is exposed over similar to 1.6 km vertically and has the shape of to inverted cop with distinct metal zoning. Fluid inclusions in the barren but highly veined and potassically altered deep center of the system have intermediate density (similar to 0.6 g cm(-3)) and a salinity of similar to 7 wt percent NaCl equiv. They have subequal concentrations of Na, K, Fe, Cu and contain minor CO(2). The intermediate-density fluids were trapped as a single phase, mostly at \u0026amp;gt;500 degrees C and \u0026amp;gt;800 bars. The Au-Cu-rich center near the top of the orebody contains low-density vapor inclusions (similar to 0.2 g cm(-3)) coexisting with brine inclusions containing similar to 45 wt. percent NaCl equiv. The vertical transition Of different inclusion types indicates phase separation of the single-phase input fluid upon volume expansion associated with a pressure drop to 200 +/- 100 liars. Mass-balance calculation based on all analyzed inclusion components indicates that the mass of the vapor phase exceeded that of the brine by similar to 9/1. The vapor contained Cu as its dominant cation (similar to 1.5 wt%) and contributed about 9.5 percent of the total amount of copper transported to the base of the orebody. Bornite. chalcopyrite, and native gold were precipitated in a narrow temperature interval from 430 degrees to 350 degrees C, into secondary pore space created by local redissolution of vein quartz as a result id quartz solubility in the vapor-dominated fluid system. Intermediate-density fluid inclusions in the deepest parts of the peripheral copper ore zone have identical density and composition, including similar gold contents, as those in the deep center. Microthermometry and statistical estimation of phase proportions in the inclusions show that the vapor in the peripheral Cu-rich but Au-poor ore zone remained denser, and the separating brine was less saline (similar to 36 wt% NaCl equiv), compared to vapor and brine in the central Au-Cu ore zone. This indicates that the peripheral fluids experienced a lower degree of phase separation, due to slightly higher fluid pressure at equivalent temperature, compared to more strongly expanding fluids in the center oldie system. The systematic zoning or Au/Cu within the ore shell, despite compositionally similar input Hinds. is interpreted to have resulted from slightly different pressure-temperature-density evolution paths of magmatic fluids. Copper was selectively precipitated in the peripheral ore zone, in contrast to complete coprecipitation of Au and Cu ill the central upflow zone of the vapor plume. The formation of particularly rich Cu-Au ore in the center of the upward-expanding fluid plume is consistent with published experimental data, showing that the solubility metals in hydrous vapor decreases sharply with falling pressure. due to destabilization of the hydration shell around metal complexes in expanding vapor. This interpretation supports the classic vapor plume model for porphyry clipper ore formation but additionally emphasizes the role of sulfur-bearing complexes as a key chemical control on magmatic-hydrothermal Metal transport and the deposition of Cu and Au in porphyry ores. Our interpretation of selective Cu +/- Au precipitation as a function of vapor density can explain die more general observation that most gold-rich porphyry copper deposits;tie formed in shallow sub-volcanic environments. whereas deeper scated porphyry Cu-(Mo) deposits are generally gold poor.","internal_url":"https://www.academia.edu/4938001/The_Bingham_Canyon_Porphyry_Cu_Mo_Au_Deposit_III_Zoned_Copper_Gold_Ore_Deposition_by_Magmatic_Vapor_Expansion","translated_internal_url":"","created_at":"2013-10-30T07:37:54.902-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":6486462,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"The_Bingham_Canyon_Porphyry_Cu_Mo_Au_Deposit_III_Zoned_Copper_Gold_Ore_Deposition_by_Magmatic_Vapor_Expansion","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":6486462,"first_name":"Patrick","middle_initials":null,"last_name":"Redmond","page_name":"RedmondPatrick","domain_name":"independent","created_at":"2013-10-30T07:36:46.107-07:00","display_name":"Patrick Redmond","url":"https://independent.academia.edu/RedmondPatrick"},"attachments":[],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":407,"name":"Geochemistry","url":"https://www.academia.edu/Documents/in/Geochemistry"},{"id":2406,"name":"Economic Geology","url":"https://www.academia.edu/Documents/in/Economic_Geology"},{"id":80692,"name":"Copper","url":"https://www.academia.edu/Documents/in/Copper"}],"urls":[{"id":1836444,"url":"http://econgeol.geoscienceworld.org/cgi/doi/10.2113/gsecongeo.105.1.91"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="4938000"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/4938000/Comparing_the_curriculum_development_process_in_special_MLD_schools_a_systematic_qualitative_approach"><img alt="Research paper thumbnail of Comparing the curriculum development process in special (MLD) schools: a systematic qualitative approach" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/4938000/Comparing_the_curriculum_development_process_in_special_MLD_schools_a_systematic_qualitative_approach">Comparing the curriculum development process in special (MLD) schools: a systematic qualitative approach</a></div><div class="wp-workCard_item"><span>European Journal of Special Needs Education</span><span>, 1988</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The present paper describes a comparative study of ten special schools for pupils with moderate l...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The present paper describes a comparative study of ten special schools for pupils with moderate learning difficulties in England and Wales. Qualitative analysis of interview data and curriculum documentation collected from the schools provide a model of the curriculum process which is firmly grounded in the data. Comparisons across the categories of the model indicate strong differences between the schools</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="4938000"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="4938000"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 4938000; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=4938000]").text(description); $(".js-view-count[data-work-id=4938000]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 4938000; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='4938000']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 4938000, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=4938000]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":4938000,"title":"Comparing the curriculum development process in special (MLD) schools: a systematic qualitative approach","translated_title":"","metadata":{"abstract":"The present paper describes a comparative study of ten special schools for pupils with moderate learning difficulties in England and Wales. 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