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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 John Collinson</h3></div><div class="js-work-strip profile--work_container" data-work-id="99803548"><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/99803548/Nearshore_sediment_dynamics_and_sedimentation_Edited_by_J_Hails_and_A_Carr_Wiley_London_316_pp_11_75"><img alt="Research paper thumbnail of Nearshore sediment dynamics and sedimentation, Edited by J. Hails and A. Carr, Wiley, London, 316 pp., $11.75" class="work-thumbnail" src="https://attachments.academia-assets.com/100795012/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/99803548/Nearshore_sediment_dynamics_and_sedimentation_Edited_by_J_Hails_and_A_Carr_Wiley_London_316_pp_11_75">Nearshore sediment dynamics and sedimentation, Edited by J. Hails and A. Carr, Wiley, London, 316 pp., $11.75</a></div><div class="wp-workCard_item"><span>Earth Surface Processes</span><span>, 1976</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="50b588fabd087deaae8f6b5ab50d6892" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":100795012,"asset_id":99803548,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/100795012/download_file?st=MTczMjUxMzE5MCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="99803548"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="99803548"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 99803548; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=99803548]").text(description); $(".js-view-count[data-work-id=99803548]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 99803548; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='99803548']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 99803548, 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: "50b588fabd087deaae8f6b5ab50d6892" } } $('.js-work-strip[data-work-id=99803548]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":99803548,"title":"Nearshore sediment dynamics and sedimentation, Edited by J. 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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="94297618"><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/94297618/Sedimentation_of_the_southern_part_of_the_Grindslow_shales_and_the_Kinderscout_grit"><img alt="Research paper thumbnail of Sedimentation of the southern part of the Grindslow shales and the Kinderscout grit" 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/94297618/Sedimentation_of_the_southern_part_of_the_Grindslow_shales_and_the_Kinderscout_grit">Sedimentation of the southern part of the Grindslow shales and the Kinderscout grit</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The aim of the research has been to determine the environments of deposition of the Grindslow Sha...</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 aim of the research has been to determine the environments of deposition of the Grindslow Shales and Kinderscout Grit in an area north of the Derbyshire Dome. These units overly the Mam Tor Sandstones and Shale Grit, which are thought to be turbidites showing increasing proximity to scource. The Grindslow Shales had been interpreted as the slope down which the turbidity currents were generated. Little was known of the depositional environment of the Kinderscout Grit, though shallow water conditions had been suggested. The sequence, from the base of the Mam Tor Sandstones to the top of the Kinderscout Grit, falls within the zone R 1 c of the Namurian. The outcrops of the Kinderscout Plateau, Derwentdale and Longendale have been mapped and numerous sections measured. In all, 17 facies have been recognised, described and interpreted in hydrodynamic terms on the basis of their internal evidence. Three silts tone facies and one of silty sandstone are thought to be largely deposited f...</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="94297618"><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="94297618"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 94297618; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=94297618]").text(description); $(".js-view-count[data-work-id=94297618]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 94297618; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='94297618']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 94297618, 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" } } $('.js-work-strip[data-work-id=94297618]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":94297618,"title":"Sedimentation of the southern part of the Grindslow shales and the Kinderscout grit","translated_title":"","metadata":{"abstract":"The aim of the research has been to determine the environments of deposition of the Grindslow Shales and Kinderscout Grit in an area north of the Derbyshire Dome. 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Three silts tone facies and one of silty sandstone are thought to be largely deposited f...","publication_date":{"day":null,"month":null,"year":1967,"errors":{}}},"translated_abstract":"The aim of the research has been to determine the environments of deposition of the Grindslow Shales and Kinderscout Grit in an area north of the Derbyshire Dome. These units overly the Mam Tor Sandstones and Shale Grit, which are thought to be turbidites showing increasing proximity to scource. The Grindslow Shales had been interpreted as the slope down which the turbidity currents were generated. Little was known of the depositional environment of the Kinderscout Grit, though shallow water conditions had been suggested. The sequence, from the base of the Mam Tor Sandstones to the top of the Kinderscout Grit, falls within the zone R 1 c of the Namurian. The outcrops of the Kinderscout Plateau, Derwentdale and Longendale have been mapped and numerous sections measured. In all, 17 facies have been recognised, described and interpreted in hydrodynamic terms on the basis of their internal evidence. Three silts tone facies and one of silty sandstone are thought to be largely deposited f...","internal_url":"https://www.academia.edu/94297618/Sedimentation_of_the_southern_part_of_the_Grindslow_shales_and_the_Kinderscout_grit","translated_internal_url":"","created_at":"2023-01-03T23:57:13.545-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":24658242,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Sedimentation_of_the_southern_part_of_the_Grindslow_shales_and_the_Kinderscout_grit","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":24658242,"first_name":"John","middle_initials":"","last_name":"Collinson","page_name":"CollinsonJohn","domain_name":"independent","created_at":"2015-01-11T08:00:35.892-08:00","display_name":"John Collinson","url":"https://independent.academia.edu/CollinsonJohn"},"attachments":[],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":197271,"name":"University of Oxford","url":"https://www.academia.edu/Documents/in/University_of_Oxford"},{"id":318566,"name":"Sedimentation","url":"https://www.academia.edu/Documents/in/Sedimentation"},{"id":785026,"name":"GRIT","url":"https://www.academia.edu/Documents/in/GRIT"}],"urls":[]}, 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="83631281"><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/83631281/The_Haslingden_Flags_Namurian_G1_of_South_East_Lancashire_Bar_Finger_Sands_in_the_Pennine_Basin"><img alt="Research paper thumbnail of The Haslingden Flags (Namurian G1) of South-East Lancashire: Bar Finger Sands in the Pennine Basin" 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/83631281/The_Haslingden_Flags_Namurian_G1_of_South_East_Lancashire_Bar_Finger_Sands_in_the_Pennine_Basin">The Haslingden Flags (Namurian G1) of South-East Lancashire: Bar Finger Sands in the Pennine Basin</a></div><div class="wp-workCard_item"><span>Proceedings of the Yorkshire Geological Society</span><span>, 1975</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Summary The sedimentary sequence between the Gastrioceras cancellatum Marine Band and the Rough R...</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">Summary The sedimentary sequence between the Gastrioceras cancellatum Marine Band and the Rough Rock in south-east Lancashire comprises a wide range of lithologies ranging from mudstone through siltstone to ripple cross-laminated and cross-bedded medium-grained sandstones. The sequence consists broadly of two coarsening upwards sequences, each dominantly of mudstone and siltstone in its lower part and each capped by a sandstone member, the Lower and Upper Haslingden Flags respectively. Isopachytes on these sandstones show them to form elongate lobes thinning eastwards from a maximum exposed development around Blackburn. Palaeocurrent directions are dominantly towards the east. Both sandstones are cross-bedded in their central upstream regions and, in the Upper Haslingden Flags, a complex internal geometry involves large scale, low-angle cross-bedding up to 27 metres thick. The overall geometry and lithofacies assemblage is compared with that of a modern bar-finger sand and, in the Upper Haslingden Flags, the internal structure of the actual distributary mouth bar is shown. These deltas differ in type from the usual Millstone Grit delta in their finer grain size, their body geometry and in their palaeocurrent pattern. These points of difference raise the possibility of a western source area for at least some of the Millstone Grit and also imply that a different hydrological regime may have operated there.</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="83631281"><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="83631281"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 83631281; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=83631281]").text(description); $(".js-view-count[data-work-id=83631281]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 83631281; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='83631281']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 83631281, 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" } } $('.js-work-strip[data-work-id=83631281]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":83631281,"title":"The Haslingden Flags (Namurian G1) of South-East Lancashire: Bar Finger Sands in the Pennine Basin","translated_title":"","metadata":{"abstract":"Summary The sedimentary sequence between the Gastrioceras cancellatum Marine Band and the Rough Rock in south-east Lancashire comprises a wide range of lithologies ranging from mudstone through siltstone to ripple cross-laminated and cross-bedded medium-grained sandstones. The sequence consists broadly of two coarsening upwards sequences, each dominantly of mudstone and siltstone in its lower part and each capped by a sandstone member, the Lower and Upper Haslingden Flags respectively. Isopachytes on these sandstones show them to form elongate lobes thinning eastwards from a maximum exposed development around Blackburn. Palaeocurrent directions are dominantly towards the east. Both sandstones are cross-bedded in their central upstream regions and, in the Upper Haslingden Flags, a complex internal geometry involves large scale, low-angle cross-bedding up to 27 metres thick. The overall geometry and lithofacies assemblage is compared with that of a modern bar-finger sand and, in the Upper Haslingden Flags, the internal structure of the actual distributary mouth bar is shown. These deltas differ in type from the usual Millstone Grit delta in their finer grain size, their body geometry and in their palaeocurrent pattern. 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Isopachytes on these sandstones show them to form elongate lobes thinning eastwards from a maximum exposed development around Blackburn. Palaeocurrent directions are dominantly towards the east. Both sandstones are cross-bedded in their central upstream regions and, in the Upper Haslingden Flags, a complex internal geometry involves large scale, low-angle cross-bedding up to 27 metres thick. The overall geometry and lithofacies assemblage is compared with that of a modern bar-finger sand and, in the Upper Haslingden Flags, the internal structure of the actual distributary mouth bar is shown. These deltas differ in type from the usual Millstone Grit delta in their finer grain size, their body geometry and in their palaeocurrent pattern. These points of difference raise the possibility of a western source area for at least some of the Millstone Grit and also imply that a different hydrological regime may have operated there.","internal_url":"https://www.academia.edu/83631281/The_Haslingden_Flags_Namurian_G1_of_South_East_Lancashire_Bar_Finger_Sands_in_the_Pennine_Basin","translated_internal_url":"","created_at":"2022-07-24T00:05:16.675-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":24658242,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"The_Haslingden_Flags_Namurian_G1_of_South_East_Lancashire_Bar_Finger_Sands_in_the_Pennine_Basin","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":24658242,"first_name":"John","middle_initials":"","last_name":"Collinson","page_name":"CollinsonJohn","domain_name":"independent","created_at":"2015-01-11T08:00:35.892-08:00","display_name":"John Collinson","url":"https://independent.academia.edu/CollinsonJohn"},"attachments":[],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"}],"urls":[]}, dispatcherData: dispatcherData }); 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INFORMS provides unique networking and learning opportunities for individual professionals, and organizations of all types and sizes, to better understand and use O.R. and analytics tools and methods to transform strategic visions and achieve better outcomes. 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L. Banks and J. D. Collinson" class="work-thumbnail" src="https://attachments.academia-assets.com/88078648/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/82335747/Some_sedimentological_aspects_of_planar_cross_stratification_in_a_sandy_braided_river_a_reply_to_N_L_Banks_and_J_D_Collinson">Some sedimentological aspects of planar cross-stratification in a sandy braided river; a reply to N. L. Banks and J. D. Collinson</a></div><div class="wp-workCard_item"><span>Journal of Sedimentary Research</span><span>, 1974</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="616f7ecc4b1e0a480f9d6fd38c481ce7" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":88078648,"asset_id":82335747,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/88078648/download_file?st=MTczMjUxMzE5MCw4LjIyMi4yMDguMTQ2&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="82335747"><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="82335747"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 82335747; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=82335747]").text(description); $(".js-view-count[data-work-id=82335747]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 82335747; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='82335747']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 82335747, 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: "616f7ecc4b1e0a480f9d6fd38c481ce7" } } $('.js-work-strip[data-work-id=82335747]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":82335747,"title":"Some sedimentological aspects of planar cross-stratification in a sandy braided river; a reply to N. L. Banks and J. D. Collinson","translated_title":"","metadata":{"publisher":"Society for Sedimentary Geology","grobid_abstract":"Tabular sets of planar cross-stratlfication are characteristic structures produced by transverse bars in the sand-bed Platte River in Nebraska. Certain sedimentologic characteristics of the Platte bars provide potentially useful information for interpreting the origin of planar cross-strata in ancient deposits. Alternating coarse and flue-graded foreset laminations result from continuous avalanching at bar margins of sediment previously sorted by small scale bed forms on the bar surface. Surface dune transport yields thicker and more distinct coarse-fine foreset laminae than ripples. Foreset angles of inclination tend to decrease with increasing flow regime. Several structures are produced at active bar margins swept by side currents, including ripples and dunes perpendicular to the bar slip face, foreset spurs, and straight-crested ripples on the slip face. Each of these structures produce small scale cross-stratification oriented at high angles to the associated planar cross-bed. Large differences between current and foreset dip azimuths frequently occur because of the irregular and lobate shapes of transverse bars. Only 30.5% of the bar foreset directions correspond to within 5 ° of the currents that formed them. Foreset dip azimuths in a straight 2.1-kin reach of the ]ou-er Platte are widely dispersed, although their vector mean accurately identifies the direction of the main channel complex. Planar cross-bed orientations computed for the entire Platte plus the Nebraska portion of the South Platte yielded a variance of 6,129 and a vector magnitude of 35.6%, indicating dispersions greater than commonly assumed for braided streams. 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A. Read" class="work-thumbnail" src="https://attachments.academia-assets.com/86164344/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/79455070/Discussion_of_The_Millstone_Grit_Namurian_of_the_southern_Pennines_viewed_in_the_light_of_eustatically_controlled_sequence_stratigraphy_by_W_A_Read">Discussion of: ‘The Millstone Grit (Namurian) of the southern Pennines viewed in the light of eustatically controlled sequence stratigraphy’ by W. A. Read</a></div><div class="wp-workCard_item"><span>Geological Journal</span><span>, 1992</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="009d37b423c0c2df055635f4c96f264e" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":86164344,"asset_id":79455070,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/86164344/download_file?st=MTczMjUxMzE5MCw4LjIyMi4yMDguMTQ2&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="79455070"><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="79455070"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 79455070; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=79455070]").text(description); $(".js-view-count[data-work-id=79455070]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 79455070; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='79455070']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 79455070, 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: "009d37b423c0c2df055635f4c96f264e" } } $('.js-work-strip[data-work-id=79455070]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":79455070,"title":"Discussion of: ‘The Millstone Grit (Namurian) of the southern Pennines viewed in the light of eustatically controlled sequence stratigraphy’ by W. 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Journal of Sedimentary Petrology Vol. 44 ( 1974 ) No...</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">PDF Click to view page images in PDF format. Journal of Sedimentary Petrology Vol. 44 ( 1974 ) No. 1. (March), Pages 265-267. Some Sedimentological Aspects of Planar Cross-stratification in a Sandy Braided River: DISCUSSION. Nigel L. Banks, John 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="77668312"><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/77668312/Discussion_of_some_sedimentological_aspects_of_planar_cross_stratification_in_a_sandy_braided_river"><img alt="Research paper thumbnail of Discussion of "some sedimentological aspects of planar cross-stratification in a sandy braided river" 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/77668312/Discussion_of_some_sedimentological_aspects_of_planar_cross_stratification_in_a_sandy_braided_river">Discussion of "some sedimentological aspects of planar cross-stratification in a sandy braided river</a></div><div class="wp-workCard_item"><span>Journal of Sedimentary Research</span><span>, 1974</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Page 1. I) ISCUSSIONS 265 I urge that &amp;amp;quot;orthoquartzite&amp;amp;quot; be standardized ...</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">Page 1. I) ISCUSSIONS 265 I urge that &amp;amp;quot;orthoquartzite&amp;amp;quot; be standardized according to its original meaning for a rock composed chiefly of quartz so tightly cemented with silica by ground water or non-tectonic processes that it breaks across the constituent grains. ...</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="77668312"><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="77668312"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 77668312; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=77668312]").text(description); $(".js-view-count[data-work-id=77668312]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 77668312; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='77668312']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 77668312, 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" } } $('.js-work-strip[data-work-id=77668312]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":77668312,"title":"Discussion of \"some sedimentological aspects of planar cross-stratification in a sandy braided river","translated_title":"","metadata":{"abstract":"Page 1. 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A series of 21 vertical sections were measured with dip and azimuth (dip-log) readings taken every 0.2 m, which were calibrated to previously described sedimentological sections and recordings of surface natural gamma ray profiles. The inter-relationship between the scale of sedimentary structures and dipmeter processing parameters is shown by dip-log measurements in medium scale, crossbedded sedimentary structures. The analysis of grouped dip-log data is seen to give palaeocurrents very similar to those measured by traditional methods at outcrop. The relationship between sedimentological facies and ‘dip-log facies’ is applied to reservoir characterization, and statistical analysis of dip-log data is demonstrated to be an aid to inter-well comparisons. Analysis techniques, mainly computer based and applicable in the subsurface, are applied to the outcrop data and the implications for subsurface dipmeter studies are stressed.</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="77668311"><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="77668311"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 77668311; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=77668311]").text(description); $(".js-view-count[data-work-id=77668311]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 77668311; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='77668311']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 77668311, 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" } } $('.js-work-strip[data-work-id=77668311]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":77668311,"title":"Analogue dipmeter logs through a prograding deltaic sandbody","translated_title":"","metadata":{"abstract":"Abstract Detailed analogue dipmeter measurements have been made along a 430 m roadcut in the Upper Namurian Rough Rock at Elland in Yorkshire. 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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="94297618"><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/94297618/Sedimentation_of_the_southern_part_of_the_Grindslow_shales_and_the_Kinderscout_grit"><img alt="Research paper thumbnail of Sedimentation of the southern part of the Grindslow shales and the Kinderscout grit" 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/94297618/Sedimentation_of_the_southern_part_of_the_Grindslow_shales_and_the_Kinderscout_grit">Sedimentation of the southern part of the Grindslow shales and the Kinderscout grit</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The aim of the research has been to determine the environments of deposition of the Grindslow Sha...</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 aim of the research has been to determine the environments of deposition of the Grindslow Shales and Kinderscout Grit in an area north of the Derbyshire Dome. These units overly the Mam Tor Sandstones and Shale Grit, which are thought to be turbidites showing increasing proximity to scource. The Grindslow Shales had been interpreted as the slope down which the turbidity currents were generated. Little was known of the depositional environment of the Kinderscout Grit, though shallow water conditions had been suggested. The sequence, from the base of the Mam Tor Sandstones to the top of the Kinderscout Grit, falls within the zone R 1 c of the Namurian. The outcrops of the Kinderscout Plateau, Derwentdale and Longendale have been mapped and numerous sections measured. In all, 17 facies have been recognised, described and interpreted in hydrodynamic terms on the basis of their internal evidence. 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Three silts tone facies and one of silty sandstone are thought to be largely deposited f...","publication_date":{"day":null,"month":null,"year":1967,"errors":{}}},"translated_abstract":"The aim of the research has been to determine the environments of deposition of the Grindslow Shales and Kinderscout Grit in an area north of the Derbyshire Dome. These units overly the Mam Tor Sandstones and Shale Grit, which are thought to be turbidites showing increasing proximity to scource. The Grindslow Shales had been interpreted as the slope down which the turbidity currents were generated. Little was known of the depositional environment of the Kinderscout Grit, though shallow water conditions had been suggested. The sequence, from the base of the Mam Tor Sandstones to the top of the Kinderscout Grit, falls within the zone R 1 c of the Namurian. The outcrops of the Kinderscout Plateau, Derwentdale and Longendale have been mapped and numerous sections measured. In all, 17 facies have been recognised, described and interpreted in hydrodynamic terms on the basis of their internal evidence. Three silts tone facies and one of silty sandstone are thought to be largely deposited f...","internal_url":"https://www.academia.edu/94297618/Sedimentation_of_the_southern_part_of_the_Grindslow_shales_and_the_Kinderscout_grit","translated_internal_url":"","created_at":"2023-01-03T23:57:13.545-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":24658242,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Sedimentation_of_the_southern_part_of_the_Grindslow_shales_and_the_Kinderscout_grit","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":24658242,"first_name":"John","middle_initials":"","last_name":"Collinson","page_name":"CollinsonJohn","domain_name":"independent","created_at":"2015-01-11T08:00:35.892-08:00","display_name":"John Collinson","url":"https://independent.academia.edu/CollinsonJohn"},"attachments":[],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":197271,"name":"University of Oxford","url":"https://www.academia.edu/Documents/in/University_of_Oxford"},{"id":318566,"name":"Sedimentation","url":"https://www.academia.edu/Documents/in/Sedimentation"},{"id":785026,"name":"GRIT","url":"https://www.academia.edu/Documents/in/GRIT"}],"urls":[]}, 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="83631281"><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/83631281/The_Haslingden_Flags_Namurian_G1_of_South_East_Lancashire_Bar_Finger_Sands_in_the_Pennine_Basin"><img alt="Research paper thumbnail of The Haslingden Flags (Namurian G1) of South-East Lancashire: Bar Finger Sands in the Pennine Basin" 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/83631281/The_Haslingden_Flags_Namurian_G1_of_South_East_Lancashire_Bar_Finger_Sands_in_the_Pennine_Basin">The Haslingden Flags (Namurian G1) of South-East Lancashire: Bar Finger Sands in the Pennine Basin</a></div><div class="wp-workCard_item"><span>Proceedings of the Yorkshire Geological Society</span><span>, 1975</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Summary The sedimentary sequence between the Gastrioceras cancellatum Marine Band and the Rough R...</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">Summary The sedimentary sequence between the Gastrioceras cancellatum Marine Band and the Rough Rock in south-east Lancashire comprises a wide range of lithologies ranging from mudstone through siltstone to ripple cross-laminated and cross-bedded medium-grained sandstones. The sequence consists broadly of two coarsening upwards sequences, each dominantly of mudstone and siltstone in its lower part and each capped by a sandstone member, the Lower and Upper Haslingden Flags respectively. Isopachytes on these sandstones show them to form elongate lobes thinning eastwards from a maximum exposed development around Blackburn. Palaeocurrent directions are dominantly towards the east. Both sandstones are cross-bedded in their central upstream regions and, in the Upper Haslingden Flags, a complex internal geometry involves large scale, low-angle cross-bedding up to 27 metres thick. The overall geometry and lithofacies assemblage is compared with that of a modern bar-finger sand and, in the Upper Haslingden Flags, the internal structure of the actual distributary mouth bar is shown. These deltas differ in type from the usual Millstone Grit delta in their finer grain size, their body geometry and in their palaeocurrent pattern. These points of difference raise the possibility of a western source area for at least some of the Millstone Grit and also imply that a different hydrological regime may have operated there.</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="83631281"><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="83631281"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 83631281; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=83631281]").text(description); $(".js-view-count[data-work-id=83631281]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 83631281; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='83631281']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 83631281, 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" } } $('.js-work-strip[data-work-id=83631281]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":83631281,"title":"The Haslingden Flags (Namurian G1) of South-East Lancashire: Bar Finger Sands in the Pennine Basin","translated_title":"","metadata":{"abstract":"Summary The sedimentary sequence between the Gastrioceras cancellatum Marine Band and the Rough Rock in south-east Lancashire comprises a wide range of lithologies ranging from mudstone through siltstone to ripple cross-laminated and cross-bedded medium-grained sandstones. The sequence consists broadly of two coarsening upwards sequences, each dominantly of mudstone and siltstone in its lower part and each capped by a sandstone member, the Lower and Upper Haslingden Flags respectively. Isopachytes on these sandstones show them to form elongate lobes thinning eastwards from a maximum exposed development around Blackburn. Palaeocurrent directions are dominantly towards the east. Both sandstones are cross-bedded in their central upstream regions and, in the Upper Haslingden Flags, a complex internal geometry involves large scale, low-angle cross-bedding up to 27 metres thick. The overall geometry and lithofacies assemblage is compared with that of a modern bar-finger sand and, in the Upper Haslingden Flags, the internal structure of the actual distributary mouth bar is shown. These deltas differ in type from the usual Millstone Grit delta in their finer grain size, their body geometry and in their palaeocurrent pattern. These points of difference raise the possibility of a western source area for at least some of the Millstone Grit and also imply that a different hydrological regime may have operated there.","publisher":"Geological Society of London","publication_date":{"day":null,"month":null,"year":1975,"errors":{}},"publication_name":"Proceedings of the Yorkshire Geological Society"},"translated_abstract":"Summary The sedimentary sequence between the Gastrioceras cancellatum Marine Band and the Rough Rock in south-east Lancashire comprises a wide range of lithologies ranging from mudstone through siltstone to ripple cross-laminated and cross-bedded medium-grained sandstones. The sequence consists broadly of two coarsening upwards sequences, each dominantly of mudstone and siltstone in its lower part and each capped by a sandstone member, the Lower and Upper Haslingden Flags respectively. Isopachytes on these sandstones show them to form elongate lobes thinning eastwards from a maximum exposed development around Blackburn. Palaeocurrent directions are dominantly towards the east. Both sandstones are cross-bedded in their central upstream regions and, in the Upper Haslingden Flags, a complex internal geometry involves large scale, low-angle cross-bedding up to 27 metres thick. The overall geometry and lithofacies assemblage is compared with that of a modern bar-finger sand and, in the Upper Haslingden Flags, the internal structure of the actual distributary mouth bar is shown. These deltas differ in type from the usual Millstone Grit delta in their finer grain size, their body geometry and in their palaeocurrent pattern. These points of difference raise the possibility of a western source area for at least some of the Millstone Grit and also imply that a different hydrological regime may have operated there.","internal_url":"https://www.academia.edu/83631281/The_Haslingden_Flags_Namurian_G1_of_South_East_Lancashire_Bar_Finger_Sands_in_the_Pennine_Basin","translated_internal_url":"","created_at":"2022-07-24T00:05:16.675-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":24658242,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"The_Haslingden_Flags_Namurian_G1_of_South_East_Lancashire_Bar_Finger_Sands_in_the_Pennine_Basin","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":24658242,"first_name":"John","middle_initials":"","last_name":"Collinson","page_name":"CollinsonJohn","domain_name":"independent","created_at":"2015-01-11T08:00:35.892-08:00","display_name":"John Collinson","url":"https://independent.academia.edu/CollinsonJohn"},"attachments":[],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"}],"urls":[]}, dispatcherData: dispatcherData }); 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For more information on INFORMS, its publications, membership, or meetings visit http://www.informs.org","publication_date":{"day":null,"month":null,"year":1975,"errors":{}},"publication_name":"Sedimentology","grobid_abstract_attachment_id":88598529},"translated_abstract":null,"internal_url":"https://www.academia.edu/83152080/The_size_and_shape_of_small_scale_current_ripples_an_experimental_study_using_medium_sand","translated_internal_url":"","created_at":"2022-07-14T11:57:54.483-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":24658242,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":88598529,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/88598529/thumbnails/1.jpg","file_name":"msom.1100.pdf","download_url":"https://www.academia.edu/attachments/88598529/download_file?st=MTczMjUxMzE5MCw4LjIyMi4yMDguMTQ2&st=MTczMjUxMzE5MCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"The_size_and_shape_of_small_scale_curren.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/88598529/msom.1100-libre.pdf?1657839144=\u0026response-content-disposition=attachment%3B+filename%3DThe_size_and_shape_of_small_scale_curren.pdf\u0026Expires=1732516790\u0026Signature=doe8FcVjV2xzuvk0~jcPIRwZ5J6J0k82AnyfethnI2uZaYd7cIuPb1c5pC-h~bjrW1s3wjFdcWrSJ1z11Ap0BcQ6g3ruT214pokIBDZsEFShtzg5b5ztb6IeqtEgwZKZeYu0cL7pOzbYzCln5-3Z-eCJNyzb5GLMBuD~z10gnCYozdEAHYzB6-bstQ1zHbj2NjYwsN9c4rRkRUWjw80Mc89aeP4hSxO7LWL6QBmnzZic1WV9B6bNJMTTcLB5PYuTOhVrIBymF~O7FselXY~abgKysfoTiBnURraZY3x-1lF1z-hrkuZCdZIf58ENNS7gs4Wu8vCntlbtZzWYw7f6~w__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"The_size_and_shape_of_small_scale_current_ripples_an_experimental_study_using_medium_sand","translated_slug":"","page_count":6,"language":"en","content_type":"Work","owner":{"id":24658242,"first_name":"John","middle_initials":"","last_name":"Collinson","page_name":"CollinsonJohn","domain_name":"independent","created_at":"2015-01-11T08:00:35.892-08:00","display_name":"John Collinson","url":"https://independent.academia.edu/CollinsonJohn"},"attachments":[{"id":88598529,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/88598529/thumbnails/1.jpg","file_name":"msom.1100.pdf","download_url":"https://www.academia.edu/attachments/88598529/download_file?st=MTczMjUxMzE5MCw4LjIyMi4yMDguMTQ2&st=MTczMjUxMzE5MCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"The_size_and_shape_of_small_scale_curren.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/88598529/msom.1100-libre.pdf?1657839144=\u0026response-content-disposition=attachment%3B+filename%3DThe_size_and_shape_of_small_scale_curren.pdf\u0026Expires=1732516790\u0026Signature=doe8FcVjV2xzuvk0~jcPIRwZ5J6J0k82AnyfethnI2uZaYd7cIuPb1c5pC-h~bjrW1s3wjFdcWrSJ1z11Ap0BcQ6g3ruT214pokIBDZsEFShtzg5b5ztb6IeqtEgwZKZeYu0cL7pOzbYzCln5-3Z-eCJNyzb5GLMBuD~z10gnCYozdEAHYzB6-bstQ1zHbj2NjYwsN9c4rRkRUWjw80Mc89aeP4hSxO7LWL6QBmnzZic1WV9B6bNJMTTcLB5PYuTOhVrIBymF~O7FselXY~abgKysfoTiBnURraZY3x-1lF1z-hrkuZCdZIf58ENNS7gs4Wu8vCntlbtZzWYw7f6~w__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":420,"name":"Sedimentology","url":"https://www.academia.edu/Documents/in/Sedimentology"},{"id":215075,"name":"Experimental Study","url":"https://www.academia.edu/Documents/in/Experimental_Study"}],"urls":[{"id":22173460,"url":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1365-3091.1975.tb00247.x"}]}, 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="82335747"><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/82335747/Some_sedimentological_aspects_of_planar_cross_stratification_in_a_sandy_braided_river_a_reply_to_N_L_Banks_and_J_D_Collinson"><img alt="Research paper thumbnail of Some sedimentological aspects of planar cross-stratification in a sandy braided river; a reply to N. L. Banks and J. D. Collinson" class="work-thumbnail" src="https://attachments.academia-assets.com/88078648/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/82335747/Some_sedimentological_aspects_of_planar_cross_stratification_in_a_sandy_braided_river_a_reply_to_N_L_Banks_and_J_D_Collinson">Some sedimentological aspects of planar cross-stratification in a sandy braided river; a reply to N. L. Banks and J. D. Collinson</a></div><div class="wp-workCard_item"><span>Journal of Sedimentary Research</span><span>, 1974</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="616f7ecc4b1e0a480f9d6fd38c481ce7" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":88078648,"asset_id":82335747,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/88078648/download_file?st=MTczMjUxMzE5MCw4LjIyMi4yMDguMTQ2&st=MTczMjUxMzE5MCw4LjIyMi4yMDguMTQ2&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="82335747"><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="82335747"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 82335747; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=82335747]").text(description); $(".js-view-count[data-work-id=82335747]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 82335747; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='82335747']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 82335747, 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: "616f7ecc4b1e0a480f9d6fd38c481ce7" } } $('.js-work-strip[data-work-id=82335747]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":82335747,"title":"Some sedimentological aspects of planar cross-stratification in a sandy braided river; a reply to N. L. Banks and J. D. Collinson","translated_title":"","metadata":{"publisher":"Society for Sedimentary Geology","grobid_abstract":"Tabular sets of planar cross-stratlfication are characteristic structures produced by transverse bars in the sand-bed Platte River in Nebraska. Certain sedimentologic characteristics of the Platte bars provide potentially useful information for interpreting the origin of planar cross-strata in ancient deposits. Alternating coarse and flue-graded foreset laminations result from continuous avalanching at bar margins of sediment previously sorted by small scale bed forms on the bar surface. Surface dune transport yields thicker and more distinct coarse-fine foreset laminae than ripples. Foreset angles of inclination tend to decrease with increasing flow regime. Several structures are produced at active bar margins swept by side currents, including ripples and dunes perpendicular to the bar slip face, foreset spurs, and straight-crested ripples on the slip face. Each of these structures produce small scale cross-stratification oriented at high angles to the associated planar cross-bed. Large differences between current and foreset dip azimuths frequently occur because of the irregular and lobate shapes of transverse bars. Only 30.5% of the bar foreset directions correspond to within 5 ° of the currents that formed them. Foreset dip azimuths in a straight 2.1-kin reach of the ]ou-er Platte are widely dispersed, although their vector mean accurately identifies the direction of the main channel complex. Planar cross-bed orientations computed for the entire Platte plus the Nebraska portion of the South Platte yielded a variance of 6,129 and a vector magnitude of 35.6%, indicating dispersions greater than commonly assumed for braided streams. Possibilities for distinguishing planar cross-stratification formed by braided stream transverse bars from similar stratification types produced in other environments are discussed.","publication_date":{"day":null,"month":null,"year":1974,"errors":{}},"publication_name":"Journal of Sedimentary Research","grobid_abstract_attachment_id":88078648},"translated_abstract":null,"internal_url":"https://www.academia.edu/82335747/Some_sedimentological_aspects_of_planar_cross_stratification_in_a_sandy_braided_river_a_reply_to_N_L_Banks_and_J_D_Collinson","translated_internal_url":"","created_at":"2022-06-29T00:19:08.683-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":24658242,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":88078648,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/88078648/thumbnails/1.jpg","file_name":"74D725E0-2B21-11D7-8648000102C1865D20220629-1-1apoy8.pdf","download_url":"https://www.academia.edu/attachments/88078648/download_file?st=MTczMjUxMzE5MCw4LjIyMi4yMDguMTQ2&st=MTczMjUxMzE5MCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Some_sedimentological_aspects_of_planar.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/88078648/74D725E0-2B21-11D7-8648000102C1865D20220629-1-1apoy8-libre.pdf?1656487879=\u0026response-content-disposition=attachment%3B+filename%3DSome_sedimentological_aspects_of_planar.pdf\u0026Expires=1732516790\u0026Signature=ZqNjAHOe-gJ0Syamvseb1Uq~EYrNKIKtUthncZt0PJCDEySpPJjYfj-Kix5f4RBab1OGViBX2T20arO3o76~m7Vgp8cl5aOUn2mUNhsdt4ZXIt8KskjKHm8BUFHa9xaprNMgWMGtEtfUPieVrLWmg5kKs7gSMTgqU916f1EPleIdWEXJpqL3dMIUhiBkg8bZSdB1TPYOJ9lO9Ob1pDimb3AS4WHJxU0I43ey5NMKBQPHNIJVGI0GWK9q9rco3vXcsHC6iBPb97hM1f1EWdw2rRYc7g~UFs5E5xnO4vsuU0tYpyTMfrU~ogsvA0oq6f2gY8HmnffpwomvzqqRQsh8wA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Some_sedimentological_aspects_of_planar_cross_stratification_in_a_sandy_braided_river_a_reply_to_N_L_Banks_and_J_D_Collinson","translated_slug":"","page_count":11,"language":"en","content_type":"Work","owner":{"id":24658242,"first_name":"John","middle_initials":"","last_name":"Collinson","page_name":"CollinsonJohn","domain_name":"independent","created_at":"2015-01-11T08:00:35.892-08:00","display_name":"John Collinson","url":"https://independent.academia.edu/CollinsonJohn"},"attachments":[{"id":88078648,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/88078648/thumbnails/1.jpg","file_name":"74D725E0-2B21-11D7-8648000102C1865D20220629-1-1apoy8.pdf","download_url":"https://www.academia.edu/attachments/88078648/download_file?st=MTczMjUxMzE5MCw4LjIyMi4yMDguMTQ2&st=MTczMjUxMzE5MCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Some_sedimentological_aspects_of_planar.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/88078648/74D725E0-2B21-11D7-8648000102C1865D20220629-1-1apoy8-libre.pdf?1656487879=\u0026response-content-disposition=attachment%3B+filename%3DSome_sedimentological_aspects_of_planar.pdf\u0026Expires=1732516790\u0026Signature=ZqNjAHOe-gJ0Syamvseb1Uq~EYrNKIKtUthncZt0PJCDEySpPJjYfj-Kix5f4RBab1OGViBX2T20arO3o76~m7Vgp8cl5aOUn2mUNhsdt4ZXIt8KskjKHm8BUFHa9xaprNMgWMGtEtfUPieVrLWmg5kKs7gSMTgqU916f1EPleIdWEXJpqL3dMIUhiBkg8bZSdB1TPYOJ9lO9Ob1pDimb3AS4WHJxU0I43ey5NMKBQPHNIJVGI0GWK9q9rco3vXcsHC6iBPb97hM1f1EWdw2rRYc7g~UFs5E5xnO4vsuU0tYpyTMfrU~ogsvA0oq6f2gY8HmnffpwomvzqqRQsh8wA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":25436,"name":"Stratification","url":"https://www.academia.edu/Documents/in/Stratification"},{"id":1671316,"name":"Sedimentary","url":"https://www.academia.edu/Documents/in/Sedimentary"}],"urls":[]}, 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="79455070"><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/79455070/Discussion_of_The_Millstone_Grit_Namurian_of_the_southern_Pennines_viewed_in_the_light_of_eustatically_controlled_sequence_stratigraphy_by_W_A_Read"><img alt="Research paper thumbnail of Discussion of: ‘The Millstone Grit (Namurian) of the southern Pennines viewed in the light of eustatically controlled sequence stratigraphy’ by W. A. Read" class="work-thumbnail" src="https://attachments.academia-assets.com/86164344/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/79455070/Discussion_of_The_Millstone_Grit_Namurian_of_the_southern_Pennines_viewed_in_the_light_of_eustatically_controlled_sequence_stratigraphy_by_W_A_Read">Discussion of: ‘The Millstone Grit (Namurian) of the southern Pennines viewed in the light of eustatically controlled sequence stratigraphy’ by W. A. 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I) ISCUSSIONS 265 I urge that &amp;amp;quot;orthoquartzite&amp;amp;quot; be standardized ...</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">Page 1. I) ISCUSSIONS 265 I urge that &amp;amp;quot;orthoquartzite&amp;amp;quot; be standardized according to its original meaning for a rock composed chiefly of quartz so tightly cemented with silica by ground water or non-tectonic processes that it breaks across the constituent grains. ...</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="77668312"><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="77668312"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 77668312; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=77668312]").text(description); $(".js-view-count[data-work-id=77668312]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 77668312; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='77668312']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 77668312, 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" } } $('.js-work-strip[data-work-id=77668312]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":77668312,"title":"Discussion of \"some sedimentological aspects of planar cross-stratification in a sandy braided river","translated_title":"","metadata":{"abstract":"Page 1. 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I) ISCUSSIONS 265 I urge that \u0026amp;amp;quot;orthoquartzite\u0026amp;amp;quot; be standardized according to its original meaning for a rock composed chiefly of quartz so tightly cemented with silica by ground water or non-tectonic processes that it breaks across the constituent grains. ...","internal_url":"https://www.academia.edu/77668312/Discussion_of_some_sedimentological_aspects_of_planar_cross_stratification_in_a_sandy_braided_river","translated_internal_url":"","created_at":"2022-04-26T05:49:55.128-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":24658242,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Discussion_of_some_sedimentological_aspects_of_planar_cross_stratification_in_a_sandy_braided_river","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":24658242,"first_name":"John","middle_initials":"","last_name":"Collinson","page_name":"CollinsonJohn","domain_name":"independent","created_at":"2015-01-11T08:00:35.892-08:00","display_name":"John Collinson","url":"https://independent.academia.edu/CollinsonJohn"},"attachments":[],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":1671316,"name":"Sedimentary","url":"https://www.academia.edu/Documents/in/Sedimentary"}],"urls":[]}, 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="77668311"><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/77668311/Analogue_dipmeter_logs_through_a_prograding_deltaic_sandbody"><img alt="Research paper thumbnail of Analogue dipmeter logs through a prograding deltaic sandbody" 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/77668311/Analogue_dipmeter_logs_through_a_prograding_deltaic_sandbody">Analogue dipmeter logs through a prograding deltaic sandbody</a></div><div class="wp-workCard_item"><span>Geological Society, London, Special Publications</span><span>, 1992</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Abstract Detailed analogue dipmeter measurements have been made along a 430 m roadcut in the Uppe...</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 Detailed analogue dipmeter measurements have been made along a 430 m roadcut in the Upper Namurian Rough Rock at Elland in Yorkshire. A series of 21 vertical sections were measured with dip and azimuth (dip-log) readings taken every 0.2 m, which were calibrated to previously described sedimentological sections and recordings of surface natural gamma ray profiles. The inter-relationship between the scale of sedimentary structures and dipmeter processing parameters is shown by dip-log measurements in medium scale, crossbedded sedimentary structures. The analysis of grouped dip-log data is seen to give palaeocurrents very similar to those measured by traditional methods at outcrop. The relationship between sedimentological facies and ‘dip-log facies’ is applied to reservoir characterization, and statistical analysis of dip-log data is demonstrated to be an aid to inter-well comparisons. Analysis techniques, mainly computer based and applicable in the subsurface, are applied to the outcrop data and the implications for subsurface dipmeter studies are stressed.</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="77668311"><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="77668311"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 77668311; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=77668311]").text(description); $(".js-view-count[data-work-id=77668311]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 77668311; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='77668311']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 77668311, 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" } } $('.js-work-strip[data-work-id=77668311]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":77668311,"title":"Analogue dipmeter logs through a prograding deltaic sandbody","translated_title":"","metadata":{"abstract":"Abstract Detailed analogue dipmeter measurements have been made along a 430 m roadcut in the Upper Namurian Rough Rock at Elland in Yorkshire. A series of 21 vertical sections were measured with dip and azimuth (dip-log) readings taken every 0.2 m, which were calibrated to previously described sedimentological sections and recordings of surface natural gamma ray profiles. The inter-relationship between the scale of sedimentary structures and dipmeter processing parameters is shown by dip-log measurements in medium scale, crossbedded sedimentary structures. The analysis of grouped dip-log data is seen to give palaeocurrents very similar to those measured by traditional methods at outcrop. The relationship between sedimentological facies and ‘dip-log facies’ is applied to reservoir characterization, and statistical analysis of dip-log data is demonstrated to be an aid to inter-well comparisons. Analysis techniques, mainly computer based and applicable in the subsurface, are applied to the outcrop data and the implications for subsurface dipmeter studies are stressed.","publisher":"Geological Society of London","publication_date":{"day":null,"month":null,"year":1992,"errors":{}},"publication_name":"Geological Society, London, Special Publications"},"translated_abstract":"Abstract Detailed analogue dipmeter measurements have been made along a 430 m roadcut in the Upper Namurian Rough Rock at Elland in Yorkshire. A series of 21 vertical sections were measured with dip and azimuth (dip-log) readings taken every 0.2 m, which were calibrated to previously described sedimentological sections and recordings of surface natural gamma ray profiles. The inter-relationship between the scale of sedimentary structures and dipmeter processing parameters is shown by dip-log measurements in medium scale, crossbedded sedimentary structures. 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