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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 Jan-Michael Lange</h3></div><div class="js-work-strip profile--work_container" data-work-id="121074128"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/121074128/Cathodoluminescence_of_Moldavites"><img alt="Research paper thumbnail of Cathodoluminescence of Moldavites" 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" rel="nofollow" href="https://www.academia.edu/121074128/Cathodoluminescence_of_Moldavites">Cathodoluminescence of Moldavites</a></div><div class="wp-workCard_item"><span>LPICo</span><span>, Sep 1, 2015</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">A systematic study of a large set of moldavites and the application of cathodoluminescence (CL)‐s...</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">A systematic study of a large set of moldavites and the application of cathodoluminescence (CL)‐spectroscopy with a detailed discussion of spectral features is presented. Optical CL microscopy and spectroscopy (OM‐CL) were performed on 57 moldavite samples from different substrewn‐fields in Germany and the Czech Republic. The extracted CL data were supported by SEM‐EDX analysis. In general, two different kinds of CL colors can be distinguished: different shades of green in the matrix of the tektite glasses and a variation of blue color for lechatelierite inclusions (a pure silica‐glass phase). Spectral analysis of these colors shows three CL emission bands for green and five bands for blue c. Most CL activators are structural defects of the local glass network, influenced by the crystal field. The visible green CL emission is caused by defects related to strong local disorder as well as Al‐O−‐Al defects. The blue CL emission is activated by different types of lattice defects such as nonbridging oxygen‐hole center (NBOHC), self‐trapped excitons (STE), and oxygen deficiency centers (ODC). Intensity variations of the CL emissions were observed for samples from the different localities, but there is no direct correlation between substrewn‐fields and CL characteristics. Nevertheless, CL microscopy is a powerful tool for the high‐contrast visualization of internal textures such as streaks and lechatelierite in the tektite matrix due to the luminescence properties of the defect structures in the glassy network.</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="121074128"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="121074128"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 121074128; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=121074128]").text(description); $(".js-view-count[data-work-id=121074128]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 121074128; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='121074128']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=121074128]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":121074128,"title":"Cathodoluminescence of Moldavites","internal_url":"https://www.academia.edu/121074128/Cathodoluminescence_of_Moldavites","owner_id":38239714,"coauthors_can_edit":true,"owner":{"id":38239714,"first_name":"Jan-Michael","middle_initials":null,"last_name":"Lange","page_name":"janmichaellange","domain_name":"independent","created_at":"2015-11-12T22:17:29.378-08:00","display_name":"Jan-Michael Lange","url":"https://independent.academia.edu/janmichaellange"},"attachments":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="110256320"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/110256320/GeoDresden2009_Geologie_der_B%C3%B6hmischen_Masse_Regionale_und_angewandte_Geowissenschaften_in_Mitteleuropa"><img alt="Research paper thumbnail of GeoDresden2009 - Geologie der Böhmischen Masse. 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$(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="110256318"><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/110256318/The_occurrence_of_tektites_northeast_of_Dresden_Germany"><img alt="Research paper thumbnail of The occurrence of tektites northeast of Dresden, Germany" class="work-thumbnail" src="https://attachments.academia-assets.com/108129367/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/110256318/The_occurrence_of_tektites_northeast_of_Dresden_Germany">The occurrence of tektites northeast of Dresden, Germany</a></div><div class="wp-workCard_item"><span>Geochimica et Cosmochimica Acta</span><span>, Jul 1, 1992</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">About one hundred tektites have been found mainly in Tertiary fluviatile sediments in Lusatia (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">About one hundred tektites have been found mainly in Tertiary fluviatile sediments in Lusatia (northeast of Dresden). On the basis of their characteristics these tektites are more similar to those of the Moravian substrewn field than those of the Bohemian subfield; therefore, a separate Lusatian substrewn field is proposed.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="76fe7a747cd6488da1ba656f6fa9dd5e" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":108129367,"asset_id":110256318,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/108129367/download_file?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="110256318"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="110256318"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 110256318; 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="110256317"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/110256317/Scanning_Electron_Microscopy_of_Guangdong_Tektites_Exhibiting_Silica_Rich_Glass_Inclusions_and_Protrusions"><img alt="Research paper thumbnail of Scanning Electron Microscopy of Guangdong Tektites Exhibiting Silica-Rich Glass Inclusions and Protrusions" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/110256317/Scanning_Electron_Microscopy_of_Guangdong_Tektites_Exhibiting_Silica_Rich_Glass_Inclusions_and_Protrusions">Scanning Electron Microscopy of Guangdong Tektites Exhibiting Silica-Rich Glass Inclusions and Protrusions</a></div><div class="wp-workCard_item"><span>LPI</span><span>, Mar 1, 2018</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="110256317"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="110256317"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 110256317; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=110256317]").text(description); $(".js-view-count[data-work-id=110256317]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 110256317; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='110256317']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=110256317]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":110256317,"title":"Scanning Electron Microscopy of Guangdong Tektites Exhibiting Silica-Rich Glass Inclusions and Protrusions","internal_url":"https://www.academia.edu/110256317/Scanning_Electron_Microscopy_of_Guangdong_Tektites_Exhibiting_Silica_Rich_Glass_Inclusions_and_Protrusions","owner_id":38239714,"coauthors_can_edit":true,"owner":{"id":38239714,"first_name":"Jan-Michael","middle_initials":null,"last_name":"Lange","page_name":"janmichaellange","domain_name":"independent","created_at":"2015-11-12T22:17:29.378-08:00","display_name":"Jan-Michael Lange","url":"https://independent.academia.edu/janmichaellange"},"attachments":[]}, 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="110256316"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/110256316/The_chemical_variation_of_moldavite_tektites_Simple_mixing_of_terrestrial_sediments"><img alt="Research paper thumbnail of The chemical variation of moldavite tektites: Simple mixing of terrestrial sediments" 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" rel="nofollow" href="https://www.academia.edu/110256316/The_chemical_variation_of_moldavite_tektites_Simple_mixing_of_terrestrial_sediments">The chemical variation of moldavite tektites: Simple mixing of terrestrial sediments</a></div><div class="wp-workCard_item"><span>Meteoritics & Planetary Science</span><span>, Jul 1, 1997</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">— To test different hypotheses of moldavite formation, a major and trace‐element study of 25 mold...</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">— To test different hypotheses of moldavite formation, a major and trace‐element study of 25 moldavite tektites and Sm‐Nd isotope measurement of three moldavite tektites was completed. The samples were selected from the classical substrewnfields and the newly described locations in Lusatia (Saxony, Germany). Samples with unusual bulk composition were also included. The results confirm earlier studies that the variation in the chemical composition can be explained by single impact and through incomplete mixing of at least three lithographical components dominated by one of the three minerals or mineral groups: dolomite, clay minerals and quartz. An additional endmember, possibly a rare Earth&#39;s mantle component, containing high Co, Cr and Ni concentrations is also needed to explain the observed variations in compatible elements of some tektites. Volatile element abundances are low but not necessarily the result of selective volatilization.</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="110256316"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="110256316"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 110256316; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=110256316]").text(description); 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dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=110256316]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":110256316,"title":"The chemical variation of moldavite tektites: Simple mixing of terrestrial sediments","internal_url":"https://www.academia.edu/110256316/The_chemical_variation_of_moldavite_tektites_Simple_mixing_of_terrestrial_sediments","owner_id":38239714,"coauthors_can_edit":true,"owner":{"id":38239714,"first_name":"Jan-Michael","middle_initials":null,"last_name":"Lange","page_name":"janmichaellange","domain_name":"independent","created_at":"2015-11-12T22:17:29.378-08:00","display_name":"Jan-Michael Lange","url":"https://independent.academia.edu/janmichaellange"},"attachments":[]}, 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="110256315"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/110256315/Monazite_in_lithoclasts_of_suevite_impact_breccia_in_the_N%C3%B6rdlinger_Ries_Bavaria_Germany_and_its_Th_U_Pb_dating_by_electron_probe_microanalysis"><img alt="Research paper thumbnail of Monazite in lithoclasts of suevite impact breccia in the Nördlinger Ries (Bavaria, Germany) and its Th-U-Pb dating by electron probe microanalysis" 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" rel="nofollow" href="https://www.academia.edu/110256315/Monazite_in_lithoclasts_of_suevite_impact_breccia_in_the_N%C3%B6rdlinger_Ries_Bavaria_Germany_and_its_Th_U_Pb_dating_by_electron_probe_microanalysis">Monazite in lithoclasts of suevite impact breccia in the Nördlinger Ries (Bavaria, Germany) and its Th-U-Pb dating by electron probe microanalysis</a></div><div class="wp-workCard_item"><span>Zeitschrift Der Deutschen Gesellschaft Fur Geowissenschaften</span><span>, Sep 1, 2022</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="110256315"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="110256315"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 110256315; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=110256315]").text(description); $(".js-view-count[data-work-id=110256315]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 110256315; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='110256315']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=110256315]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":110256315,"title":"Monazite in lithoclasts of suevite impact breccia in the Nördlinger Ries (Bavaria, Germany) and its Th-U-Pb dating by electron probe microanalysis","internal_url":"https://www.academia.edu/110256315/Monazite_in_lithoclasts_of_suevite_impact_breccia_in_the_N%C3%B6rdlinger_Ries_Bavaria_Germany_and_its_Th_U_Pb_dating_by_electron_probe_microanalysis","owner_id":38239714,"coauthors_can_edit":true,"owner":{"id":38239714,"first_name":"Jan-Michael","middle_initials":null,"last_name":"Lange","page_name":"janmichaellange","domain_name":"independent","created_at":"2015-11-12T22:17:29.378-08:00","display_name":"Jan-Michael Lange","url":"https://independent.academia.edu/janmichaellange"},"attachments":[]}, 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="110256313"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/110256313/Apatite_fission_track_data_for_the_Postvariscan_thermotectonic_evolution_of_the_Saxon_basement_first_results"><img alt="Research paper thumbnail of Apatite fission track data for the Postvariscan thermotectonic evolution of the Saxon basement first results" 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" rel="nofollow" href="https://www.academia.edu/110256313/Apatite_fission_track_data_for_the_Postvariscan_thermotectonic_evolution_of_the_Saxon_basement_first_results">Apatite fission track data for the Postvariscan thermotectonic evolution of the Saxon basement first results</a></div><div class="wp-workCard_item"><span>Zeitschrift Der Deutschen Gesellschaft Fur Geowissenschaften</span><span>, Mar 1, 2008</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">... Im Bereich des Elbsandsteingebirges und der westli-chen Lausitz werden erstmals in den Arbeit...</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">... Im Bereich des Elbsandsteingebirges und der westli-chen Lausitz werden erstmals in den Arbeiten von Staff &amp;amp; Rassmuss (1911) und Staff (1914) Entwicklungslinien der känozoischen Morphogenese im Elbsandsteingebir-ge und in der westlichen ... (1987) mit AFT-Solve 1.2.1a ...</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="110256313"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="110256313"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 110256313; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=110256313]").text(description); $(".js-view-count[data-work-id=110256313]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 110256313; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='110256313']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=110256313]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":110256313,"title":"Apatite fission track data for the Postvariscan thermotectonic evolution of the Saxon basement first results","internal_url":"https://www.academia.edu/110256313/Apatite_fission_track_data_for_the_Postvariscan_thermotectonic_evolution_of_the_Saxon_basement_first_results","owner_id":38239714,"coauthors_can_edit":true,"owner":{"id":38239714,"first_name":"Jan-Michael","middle_initials":null,"last_name":"Lange","page_name":"janmichaellange","domain_name":"independent","created_at":"2015-11-12T22:17:29.378-08:00","display_name":"Jan-Michael Lange","url":"https://independent.academia.edu/janmichaellange"},"attachments":[]}, 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="110256311"><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/110256311/Petrographic_investigations_in_cemeteries_in_Dresden_a_scientific_view_on_the_tombstone_inventory_including_historic_and_cultural_aspects"><img alt="Research paper thumbnail of Petrographic investigations in cemeteries in Dresden: a scientific view on the tombstone inventory including historic and cultural aspects" class="work-thumbnail" src="https://attachments.academia-assets.com/108129380/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/110256311/Petrographic_investigations_in_cemeteries_in_Dresden_a_scientific_view_on_the_tombstone_inventory_including_historic_and_cultural_aspects">Petrographic investigations in cemeteries in Dresden: a scientific view on the tombstone inventory including historic and cultural aspects</a></div><div class="wp-workCard_item"><span>Environmental Earth Sciences</span><span>, Sep 1, 2018</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Cemeteries give evidence for a continuous change in sepulchral culture and provide insights into ...</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">Cemeteries give evidence for a continuous change in sepulchral culture and provide insights into the application of characteristical rock materials used for tombstones during different times. Four selected cemeteries in Dresden (the Eliasfriedhof/Elias Cemetery, the Trinitatisfriedhof/Trinity Cemetery, the Johannisfriedhof/Johannis Cemetery, and the Städtischer Urnenhain/ Municipal Urn Grove), which are of considerable cultural and historical importance, have been investigated within an ongoing mapping project. First results of this project focussing on the tombstone inventory of the mentioned graveyards and thus the use of building and decoration stones therein between 1680 and 1945 are presented in this paper. It can be demonstrated that the choice, variety, and application of rock material depends on the infrastructure and transport possibilities, but is also strongly influenced by sepulchral cultural trends and the prevailing zeitgeist. Until the middle of the 19th century, nearly solely Elbe sandstone (from the area of the Elbsandsteingebirge/Elbe sandstone mountains), that was transported on the Elbe river by ship, is found as rock material for tombstones in Dresden cemeteries. Rapid construction and development of the railway network starting around 1840 improved the availability, at first, of regional rock material (e.g., from the Lausitz/Lusatia) and, later on, from about 1880, of national and international-especially European-rock material (e.g., from Franken/Franconia, France, Scandinavia). Furthermore, the Friedhofsreformbewegung/cemetery reform movement at the beginning of the 20th century, with its significant effect on the selection of rock types used for tombstones, marks another historical breakthrough.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="e891c7550fb803b64c8312e99213deb8" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":108129380,"asset_id":110256311,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/108129380/download_file?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="110256311"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="110256311"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 110256311; 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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="110256309"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/110256309/Reply_to_Comment_by_W_von_Engelhardt_and_J_Arndt_on_The_chemical_variation_of_moldavite_tektites_Simple_mixing_of_terrestrial_sediments_"><img alt="Research paper thumbnail of Reply to Comment by W. von Engelhardt and J. Arndt on “The chemical variation of moldavite tektites: Simple mixing of terrestrial sediments”" 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" rel="nofollow" href="https://www.academia.edu/110256309/Reply_to_Comment_by_W_von_Engelhardt_and_J_Arndt_on_The_chemical_variation_of_moldavite_tektites_Simple_mixing_of_terrestrial_sediments_">Reply to Comment by W. von Engelhardt and J. Arndt on “The chemical variation of moldavite tektites: Simple mixing of terrestrial sediments”</a></div><div class="wp-workCard_item"><span>Meteoritics & Planetary Science</span><span>, May 1, 1998</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">... THOMAS MEISEL 1,* ,; JAN-MICHAEL LANGE 2. Article first published online: 4 FEB 2010. DOI: 10...</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">... THOMAS MEISEL 1,* ,; JAN-MICHAEL LANGE 2. Article first published online: 4 FEB 2010. DOI: 10.1111/j.1945-5100.1998.tb01659.x. 1998 The Meteoritical Society. ... Correspondence: THOMASMEISEL,. *Correspondence: <a href="mailto:thomas.meisel@unileoben.ac.at" rel="nofollow">thomas.meisel@unileoben.ac.at</a>. Publication History. ...</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="110256309"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="110256309"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 110256309; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=110256309]").text(description); $(".js-view-count[data-work-id=110256309]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 110256309; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='110256309']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=110256309]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":110256309,"title":"Reply to Comment by W. von Engelhardt and J. Arndt on “The chemical variation of moldavite tektites: Simple mixing of terrestrial sediments”","internal_url":"https://www.academia.edu/110256309/Reply_to_Comment_by_W_von_Engelhardt_and_J_Arndt_on_The_chemical_variation_of_moldavite_tektites_Simple_mixing_of_terrestrial_sediments_","owner_id":38239714,"coauthors_can_edit":true,"owner":{"id":38239714,"first_name":"Jan-Michael","middle_initials":null,"last_name":"Lange","page_name":"janmichaellange","domain_name":"independent","created_at":"2015-11-12T22:17:29.378-08:00","display_name":"Jan-Michael Lange","url":"https://independent.academia.edu/janmichaellange"},"attachments":[]}, 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="110256306"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/110256306/Cathodoluminescence_of_moldavites"><img alt="Research paper thumbnail of Cathodoluminescence of moldavites" 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" rel="nofollow" href="https://www.academia.edu/110256306/Cathodoluminescence_of_moldavites">Cathodoluminescence of moldavites</a></div><div class="wp-workCard_item"><span>Meteoritics & Planetary Science</span><span>, Mar 16, 2017</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">A systematic study of a large set of moldavites and the application of cathodoluminescence (CL)‐s...</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">A systematic study of a large set of moldavites and the application of cathodoluminescence (CL)‐spectroscopy with a detailed discussion of spectral features is presented. Optical CL microscopy and spectroscopy (OM‐CL) were performed on 57 moldavite samples from different substrewn‐fields in Germany and the Czech Republic. The extracted CL data were supported by SEM‐EDX analysis. In general, two different kinds of CL colors can be distinguished: different shades of green in the matrix of the tektite glasses and a variation of blue color for lechatelierite inclusions (a pure silica‐glass phase). Spectral analysis of these colors shows three CL emission bands for green and five bands for blue c. Most CL activators are structural defects of the local glass network, influenced by the crystal field. The visible green CL emission is caused by defects related to strong local disorder as well as Al‐O−‐Al defects. The blue CL emission is activated by different types of lattice defects such as nonbridging oxygen‐hole center (NBOHC), self‐trapped excitons (STE), and oxygen deficiency centers (ODC). Intensity variations of the CL emissions were observed for samples from the different localities, but there is no direct correlation between substrewn‐fields and CL characteristics. Nevertheless, CL microscopy is a powerful tool for the high‐contrast visualization of internal textures such as streaks and lechatelierite in the tektite matrix due to the luminescence properties of the defect structures in the glassy network.</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="110256306"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="110256306"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 110256306; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=110256306]").text(description); $(".js-view-count[data-work-id=110256306]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 110256306; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='110256306']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=110256306]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":110256306,"title":"Cathodoluminescence of moldavites","internal_url":"https://www.academia.edu/110256306/Cathodoluminescence_of_moldavites","owner_id":38239714,"coauthors_can_edit":true,"owner":{"id":38239714,"first_name":"Jan-Michael","middle_initials":null,"last_name":"Lange","page_name":"janmichaellange","domain_name":"independent","created_at":"2015-11-12T22:17:29.378-08:00","display_name":"Jan-Michael Lange","url":"https://independent.academia.edu/janmichaellange"},"attachments":[]}, 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="110256231"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/110256231/The_Ries_impact_and_its_distal_effects_in_sediments_of_Central_Europe_A_review"><img alt="Research paper thumbnail of The Ries impact and its distal effects in sediments of Central Europe—A review" 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" rel="nofollow" href="https://www.academia.edu/110256231/The_Ries_impact_and_its_distal_effects_in_sediments_of_Central_Europe_A_review">The Ries impact and its distal effects in sediments of Central Europe—A review</a></div><div class="wp-workCard_item"><span>Meteoritics &amp; Planetary Science</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The Ries impact is the most important cosmic event in the younger geological history of Europe. 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 Ries impact is the most important cosmic event in the younger geological history of Europe. Its effects reach far beyond the area considered so far and are documented in manifold evidence. In this paper, the widely scattered reports in the literature are compiled and supported with investigations by the authors. Besides well‐known ejecta features like the Brockhorizont, Reuter&#39;s blocks, and moldavites, little known or forgotten indications, like a lechatelierite and β‐cristobalite occurrence in Bavaria and unusual sedimentation phenomena in northern Germany, are presented. The paleogeographic reconstruction shows that the Ries impact occurred on the southern side of the Neogene Central European mainland. Large parts of this erosional area were devastated by the impact. Pressure waves and thermal radiation had a lasting effect on the landscape within hundreds of kilometers around the impact site. Destruction of the vegetation cover by impact‐induced storms, wildfires, and hea...</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="110256231"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="110256231"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 110256231; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=110256231]").text(description); $(".js-view-count[data-work-id=110256231]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 110256231; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='110256231']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=110256231]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":110256231,"title":"The Ries impact and its distal effects in sediments of Central Europe—A review","internal_url":"https://www.academia.edu/110256231/The_Ries_impact_and_its_distal_effects_in_sediments_of_Central_Europe_A_review","owner_id":38239714,"coauthors_can_edit":true,"owner":{"id":38239714,"first_name":"Jan-Michael","middle_initials":null,"last_name":"Lange","page_name":"janmichaellange","domain_name":"independent","created_at":"2015-11-12T22:17:29.378-08:00","display_name":"Jan-Michael Lange","url":"https://independent.academia.edu/janmichaellange"},"attachments":[]}, 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="108138005"><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/108138005/Die_%C3%A4ltere_Geschichte_der_Radeberger_Lik%C3%B6rfabrik_Wilhelm_Richter"><img alt="Research paper thumbnail of Die ältere Geschichte der Radeberger Likörfabrik Wilhelm Richter" class="work-thumbnail" src="https://attachments.academia-assets.com/106601605/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/108138005/Die_%C3%A4ltere_Geschichte_der_Radeberger_Lik%C3%B6rfabrik_Wilhelm_Richter">Die ältere Geschichte der Radeberger Likörfabrik Wilhelm Richter</a></div><div class="wp-workCard_item"><span>Radeberger Blätter zur Stadtgeschichte</span><span>, 2020</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Über die Vorläufer, die Gründung und die ersten Jahrzehnte der Radeberger Likörfabrik Wilhelm Ric...</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">Über die Vorläufer, die Gründung und die ersten Jahrzehnte der Radeberger Likörfabrik Wilhelm Richter existieren einige Mythen und Widersprüchlichkeiten. Anhand der Quellenlage können jedoch zahlreiche Fixpunkte in der Geschichte dieses Betriebes aufgezeigt werden, die es ermöglichen, wichtige Etappen der Firmenentwicklung bis zum Zweiten Weltkrieg in den Grundzügen zu skizzieren.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="30c7bca83ff9da27cec3daa99d411206" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":106601605,"asset_id":108138005,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/106601605/download_file?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="108138005"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="108138005"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 108138005; 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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="99211327"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/99211327/The_Ries_impact_and_its_distal_effects_in_sediments_of_Central_Europe_A_review"><img alt="Research paper thumbnail of The Ries impact and its distal effects in sediments of Central Europe—A review" 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" rel="nofollow" href="https://www.academia.edu/99211327/The_Ries_impact_and_its_distal_effects_in_sediments_of_Central_Europe_A_review">The Ries impact and its distal effects in sediments of Central Europe—A review</a></div><div class="wp-workCard_item wp-workCard--coauthors"><span>by </span><span><a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/janmichaellange">Jan-Michael Lange</a> and <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/PeterSuhr">Peter Suhr</a></span></div><div class="wp-workCard_item"><span>Meteoritics and Planetary Science</span><span>, 2023</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The Ries impact is the most important cosmic event in the younger geological history of Europe. 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 Ries impact is the most important cosmic event in the younger geological history of Europe. Its effects reach far beyond the area considered so far and are documented in manifold evidence. In this paper, the widely scattered reports in the literature are compiled and supported with investigations by the authors. Besides well-known ejecta features like the Brockhorizont, Reuter's blocks, and moldavites, little known or forgotten indications, like a lechatelierite and β-cristobalite occurrence in Bavaria and unusual sedimentation phenomena in northern Germany, are presented. The paleogeographic reconstruction shows that the Ries impact occurred on the southern side of the Neogene Central European mainland. Large parts of this erosional area were devastated by the impact. Pressure waves and thermal radiation had a lasting effect on the landscape within hundreds of kilometers around the impact site. Destruction of the vegetation cover by impact-induced storms, wildfires, and heavy rainfall generated intense erosion. The adjacent sedimentation area to the north (Paleo-North Sea) experienced an increased and short-term supply of terrestrial debris to the marine environment. The stratigraphic coincidence of these exceptional sediments with the Ries event leads us to conclude that the distal effects of the impact are present here, which have so far received little or no attention in this context. The paper considers the different indications and sets them in a large-scale context.</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="99211327"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="99211327"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 99211327; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=99211327]").text(description); 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dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=85978220]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":85978220,"title":"Die Elbe im östlichen Sachsen","internal_url":"https://www.academia.edu/85978220/Die_Elbe_im_%C3%B6stlichen_Sachsen","owner_id":38239714,"coauthors_can_edit":true,"owner":{"id":38239714,"first_name":"Jan-Michael","middle_initials":null,"last_name":"Lange","page_name":"janmichaellange","domain_name":"independent","created_at":"2015-11-12T22:17:29.378-08:00","display_name":"Jan-Michael Lange","url":"https://independent.academia.edu/janmichaellange"},"attachments":[]}, dispatcherData: dispatcherData }); $(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="4009292" id="papers"><div class="js-work-strip profile--work_container" data-work-id="121074128"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/121074128/Cathodoluminescence_of_Moldavites"><img alt="Research paper thumbnail of Cathodoluminescence of Moldavites" 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" rel="nofollow" href="https://www.academia.edu/121074128/Cathodoluminescence_of_Moldavites">Cathodoluminescence of Moldavites</a></div><div class="wp-workCard_item"><span>LPICo</span><span>, Sep 1, 2015</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">A systematic study of a large set of moldavites and the application of cathodoluminescence (CL)‐s...</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">A systematic study of a large set of moldavites and the application of cathodoluminescence (CL)‐spectroscopy with a detailed discussion of spectral features is presented. Optical CL microscopy and spectroscopy (OM‐CL) were performed on 57 moldavite samples from different substrewn‐fields in Germany and the Czech Republic. The extracted CL data were supported by SEM‐EDX analysis. In general, two different kinds of CL colors can be distinguished: different shades of green in the matrix of the tektite glasses and a variation of blue color for lechatelierite inclusions (a pure silica‐glass phase). Spectral analysis of these colors shows three CL emission bands for green and five bands for blue c. Most CL activators are structural defects of the local glass network, influenced by the crystal field. The visible green CL emission is caused by defects related to strong local disorder as well as Al‐O−‐Al defects. The blue CL emission is activated by different types of lattice defects such as nonbridging oxygen‐hole center (NBOHC), self‐trapped excitons (STE), and oxygen deficiency centers (ODC). Intensity variations of the CL emissions were observed for samples from the different localities, but there is no direct correlation between substrewn‐fields and CL characteristics. Nevertheless, CL microscopy is a powerful tool for the high‐contrast visualization of internal textures such as streaks and lechatelierite in the tektite matrix due to the luminescence properties of the defect structures in the glassy network.</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="121074128"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="121074128"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 121074128; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=121074128]").text(description); $(".js-view-count[data-work-id=121074128]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 121074128; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='121074128']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=121074128]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":121074128,"title":"Cathodoluminescence of Moldavites","internal_url":"https://www.academia.edu/121074128/Cathodoluminescence_of_Moldavites","owner_id":38239714,"coauthors_can_edit":true,"owner":{"id":38239714,"first_name":"Jan-Michael","middle_initials":null,"last_name":"Lange","page_name":"janmichaellange","domain_name":"independent","created_at":"2015-11-12T22:17:29.378-08:00","display_name":"Jan-Michael Lange","url":"https://independent.academia.edu/janmichaellange"},"attachments":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="110256320"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/110256320/GeoDresden2009_Geologie_der_B%C3%B6hmischen_Masse_Regionale_und_angewandte_Geowissenschaften_in_Mitteleuropa"><img alt="Research paper thumbnail of GeoDresden2009 - Geologie der Böhmischen Masse. 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$(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="110256318"><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/110256318/The_occurrence_of_tektites_northeast_of_Dresden_Germany"><img alt="Research paper thumbnail of The occurrence of tektites northeast of Dresden, Germany" class="work-thumbnail" src="https://attachments.academia-assets.com/108129367/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/110256318/The_occurrence_of_tektites_northeast_of_Dresden_Germany">The occurrence of tektites northeast of Dresden, Germany</a></div><div class="wp-workCard_item"><span>Geochimica et Cosmochimica Acta</span><span>, Jul 1, 1992</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">About one hundred tektites have been found mainly in Tertiary fluviatile sediments in Lusatia (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">About one hundred tektites have been found mainly in Tertiary fluviatile sediments in Lusatia (northeast of Dresden). On the basis of their characteristics these tektites are more similar to those of the Moravian substrewn field than those of the Bohemian subfield; therefore, a separate Lusatian substrewn field is proposed.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="76fe7a747cd6488da1ba656f6fa9dd5e" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":108129367,"asset_id":110256318,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/108129367/download_file?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="110256318"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="110256318"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 110256318; 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="110256317"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/110256317/Scanning_Electron_Microscopy_of_Guangdong_Tektites_Exhibiting_Silica_Rich_Glass_Inclusions_and_Protrusions"><img alt="Research paper thumbnail of Scanning Electron Microscopy of Guangdong Tektites Exhibiting Silica-Rich Glass Inclusions and Protrusions" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/110256317/Scanning_Electron_Microscopy_of_Guangdong_Tektites_Exhibiting_Silica_Rich_Glass_Inclusions_and_Protrusions">Scanning Electron Microscopy of Guangdong Tektites Exhibiting Silica-Rich Glass Inclusions and Protrusions</a></div><div class="wp-workCard_item"><span>LPI</span><span>, Mar 1, 2018</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="110256317"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="110256317"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 110256317; 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</script> <div class="js-work-strip profile--work_container" data-work-id="110256316"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/110256316/The_chemical_variation_of_moldavite_tektites_Simple_mixing_of_terrestrial_sediments"><img alt="Research paper thumbnail of The chemical variation of moldavite tektites: Simple mixing of terrestrial sediments" 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" rel="nofollow" href="https://www.academia.edu/110256316/The_chemical_variation_of_moldavite_tektites_Simple_mixing_of_terrestrial_sediments">The chemical variation of moldavite tektites: Simple mixing of terrestrial sediments</a></div><div class="wp-workCard_item"><span>Meteoritics & Planetary Science</span><span>, Jul 1, 1997</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">— To test different hypotheses of moldavite formation, a major and trace‐element study of 25 mold...</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">— To test different hypotheses of moldavite formation, a major and trace‐element study of 25 moldavite tektites and Sm‐Nd isotope measurement of three moldavite tektites was completed. The samples were selected from the classical substrewnfields and the newly described locations in Lusatia (Saxony, Germany). Samples with unusual bulk composition were also included. The results confirm earlier studies that the variation in the chemical composition can be explained by single impact and through incomplete mixing of at least three lithographical components dominated by one of the three minerals or mineral groups: dolomite, clay minerals and quartz. An additional endmember, possibly a rare Earth&#39;s mantle component, containing high Co, Cr and Ni concentrations is also needed to explain the observed variations in compatible elements of some tektites. Volatile element abundances are low but not necessarily the result of selective volatilization.</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="110256316"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="110256316"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 110256316; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=110256316]").text(description); 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} }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="110256313"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/110256313/Apatite_fission_track_data_for_the_Postvariscan_thermotectonic_evolution_of_the_Saxon_basement_first_results"><img alt="Research paper thumbnail of Apatite fission track data for the Postvariscan thermotectonic evolution of the Saxon basement first results" 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" rel="nofollow" href="https://www.academia.edu/110256313/Apatite_fission_track_data_for_the_Postvariscan_thermotectonic_evolution_of_the_Saxon_basement_first_results">Apatite fission track data for the Postvariscan thermotectonic evolution of the Saxon basement first results</a></div><div class="wp-workCard_item"><span>Zeitschrift Der Deutschen Gesellschaft Fur Geowissenschaften</span><span>, Mar 1, 2008</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">... Im Bereich des Elbsandsteingebirges und der westli-chen Lausitz werden erstmals in den Arbeit...</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">... Im Bereich des Elbsandsteingebirges und der westli-chen Lausitz werden erstmals in den Arbeiten von Staff &amp;amp; Rassmuss (1911) und Staff (1914) Entwicklungslinien der känozoischen Morphogenese im Elbsandsteingebir-ge und in der westlichen ... (1987) mit AFT-Solve 1.2.1a ...</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="110256313"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="110256313"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 110256313; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=110256313]").text(description); $(".js-view-count[data-work-id=110256313]").attr('title', description).tooltip(); 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</script> <div class="js-work-strip profile--work_container" data-work-id="110256311"><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/110256311/Petrographic_investigations_in_cemeteries_in_Dresden_a_scientific_view_on_the_tombstone_inventory_including_historic_and_cultural_aspects"><img alt="Research paper thumbnail of Petrographic investigations in cemeteries in Dresden: a scientific view on the tombstone inventory including historic and cultural aspects" class="work-thumbnail" src="https://attachments.academia-assets.com/108129380/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/110256311/Petrographic_investigations_in_cemeteries_in_Dresden_a_scientific_view_on_the_tombstone_inventory_including_historic_and_cultural_aspects">Petrographic investigations in cemeteries in Dresden: a scientific view on the tombstone inventory including historic and cultural aspects</a></div><div class="wp-workCard_item"><span>Environmental Earth Sciences</span><span>, Sep 1, 2018</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Cemeteries give evidence for a continuous change in sepulchral culture and provide insights into ...</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">Cemeteries give evidence for a continuous change in sepulchral culture and provide insights into the application of characteristical rock materials used for tombstones during different times. Four selected cemeteries in Dresden (the Eliasfriedhof/Elias Cemetery, the Trinitatisfriedhof/Trinity Cemetery, the Johannisfriedhof/Johannis Cemetery, and the Städtischer Urnenhain/ Municipal Urn Grove), which are of considerable cultural and historical importance, have been investigated within an ongoing mapping project. First results of this project focussing on the tombstone inventory of the mentioned graveyards and thus the use of building and decoration stones therein between 1680 and 1945 are presented in this paper. It can be demonstrated that the choice, variety, and application of rock material depends on the infrastructure and transport possibilities, but is also strongly influenced by sepulchral cultural trends and the prevailing zeitgeist. Until the middle of the 19th century, nearly solely Elbe sandstone (from the area of the Elbsandsteingebirge/Elbe sandstone mountains), that was transported on the Elbe river by ship, is found as rock material for tombstones in Dresden cemeteries. Rapid construction and development of the railway network starting around 1840 improved the availability, at first, of regional rock material (e.g., from the Lausitz/Lusatia) and, later on, from about 1880, of national and international-especially European-rock material (e.g., from Franken/Franconia, France, Scandinavia). Furthermore, the Friedhofsreformbewegung/cemetery reform movement at the beginning of the 20th century, with its significant effect on the selection of rock types used for tombstones, marks another historical breakthrough.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="e891c7550fb803b64c8312e99213deb8" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":108129380,"asset_id":110256311,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/108129380/download_file?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="110256311"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="110256311"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 110256311; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=110256311]").text(description); $(".js-view-count[data-work-id=110256311]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 110256311; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='110256311']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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: "e891c7550fb803b64c8312e99213deb8" } } $('.js-work-strip[data-work-id=110256311]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":110256311,"title":"Petrographic investigations in cemeteries in Dresden: a scientific view on the tombstone inventory including historic and cultural aspects","internal_url":"https://www.academia.edu/110256311/Petrographic_investigations_in_cemeteries_in_Dresden_a_scientific_view_on_the_tombstone_inventory_including_historic_and_cultural_aspects","owner_id":38239714,"coauthors_can_edit":true,"owner":{"id":38239714,"first_name":"Jan-Michael","middle_initials":null,"last_name":"Lange","page_name":"janmichaellange","domain_name":"independent","created_at":"2015-11-12T22:17:29.378-08:00","display_name":"Jan-Michael Lange","url":"https://independent.academia.edu/janmichaellange"},"attachments":[{"id":108129380,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/108129380/thumbnails/1.jpg","file_name":"s12665-018-7789-420231201-1-tmmt7j.pdf","download_url":"https://www.academia.edu/attachments/108129380/download_file","bulk_download_file_name":"Petrographic_investigations_in_cemeterie.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/108129380/s12665-018-7789-420231201-1-tmmt7j-libre.pdf?1701412837=\u0026response-content-disposition=attachment%3B+filename%3DPetrographic_investigations_in_cemeterie.pdf\u0026Expires=1740539973\u0026Signature=XuOz0Y-kxJp62-Mh~o5QlC1Zi2MXH2MPqMV2i1kWaRtpg5GGELIopH2C0Fn9FH4EDC1dw7GT-LaV5ycXdoi6ZsCl~~Yic~eBGbjdzSLmOYbuQrJWbd2lci0u6oQqelaDgUcy4eb9y5vDC4qAIeemIWnuz1AO8i2zZpMYBFwWunVpZhqy69uPQHQqLL4XlTJvkTCeQWUhF5lyHTGqN6P-38kR0TCEx9p9JiGVKzzBJSDDaysf5KOHVtikccbAa91Xyka65vS1cB5YzDZ90PP9715swn7qaMZW9xMrgp-Tt9WgrlpfbQxhwE786ezkrGxrFFQRikYZsUCs0d1SPuHIQQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}]}, 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="110256309"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/110256309/Reply_to_Comment_by_W_von_Engelhardt_and_J_Arndt_on_The_chemical_variation_of_moldavite_tektites_Simple_mixing_of_terrestrial_sediments_"><img alt="Research paper thumbnail of Reply to Comment by W. von Engelhardt and J. Arndt on “The chemical variation of moldavite tektites: Simple mixing of terrestrial sediments”" 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" rel="nofollow" href="https://www.academia.edu/110256309/Reply_to_Comment_by_W_von_Engelhardt_and_J_Arndt_on_The_chemical_variation_of_moldavite_tektites_Simple_mixing_of_terrestrial_sediments_">Reply to Comment by W. von Engelhardt and J. Arndt on “The chemical variation of moldavite tektites: Simple mixing of terrestrial sediments”</a></div><div class="wp-workCard_item"><span>Meteoritics & Planetary Science</span><span>, May 1, 1998</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">... THOMAS MEISEL 1,* ,; JAN-MICHAEL LANGE 2. Article first published online: 4 FEB 2010. DOI: 10...</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">... THOMAS MEISEL 1,* ,; JAN-MICHAEL LANGE 2. Article first published online: 4 FEB 2010. DOI: 10.1111/j.1945-5100.1998.tb01659.x. 1998 The Meteoritical Society. ... Correspondence: THOMASMEISEL,. *Correspondence: <a href="mailto:thomas.meisel@unileoben.ac.at" rel="nofollow">thomas.meisel@unileoben.ac.at</a>. Publication History. ...</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="110256309"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="110256309"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 110256309; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=110256309]").text(description); $(".js-view-count[data-work-id=110256309]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 110256309; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='110256309']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=110256309]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":110256309,"title":"Reply to Comment by W. von Engelhardt and J. Arndt on “The chemical variation of moldavite tektites: Simple mixing of terrestrial sediments”","internal_url":"https://www.academia.edu/110256309/Reply_to_Comment_by_W_von_Engelhardt_and_J_Arndt_on_The_chemical_variation_of_moldavite_tektites_Simple_mixing_of_terrestrial_sediments_","owner_id":38239714,"coauthors_can_edit":true,"owner":{"id":38239714,"first_name":"Jan-Michael","middle_initials":null,"last_name":"Lange","page_name":"janmichaellange","domain_name":"independent","created_at":"2015-11-12T22:17:29.378-08:00","display_name":"Jan-Michael Lange","url":"https://independent.academia.edu/janmichaellange"},"attachments":[]}, 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="110256306"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/110256306/Cathodoluminescence_of_moldavites"><img alt="Research paper thumbnail of Cathodoluminescence of moldavites" 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" rel="nofollow" href="https://www.academia.edu/110256306/Cathodoluminescence_of_moldavites">Cathodoluminescence of moldavites</a></div><div class="wp-workCard_item"><span>Meteoritics & Planetary Science</span><span>, Mar 16, 2017</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">A systematic study of a large set of moldavites and the application of cathodoluminescence (CL)‐s...</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">A systematic study of a large set of moldavites and the application of cathodoluminescence (CL)‐spectroscopy with a detailed discussion of spectral features is presented. Optical CL microscopy and spectroscopy (OM‐CL) were performed on 57 moldavite samples from different substrewn‐fields in Germany and the Czech Republic. The extracted CL data were supported by SEM‐EDX analysis. In general, two different kinds of CL colors can be distinguished: different shades of green in the matrix of the tektite glasses and a variation of blue color for lechatelierite inclusions (a pure silica‐glass phase). Spectral analysis of these colors shows three CL emission bands for green and five bands for blue c. Most CL activators are structural defects of the local glass network, influenced by the crystal field. The visible green CL emission is caused by defects related to strong local disorder as well as Al‐O−‐Al defects. The blue CL emission is activated by different types of lattice defects such as nonbridging oxygen‐hole center (NBOHC), self‐trapped excitons (STE), and oxygen deficiency centers (ODC). Intensity variations of the CL emissions were observed for samples from the different localities, but there is no direct correlation between substrewn‐fields and CL characteristics. Nevertheless, CL microscopy is a powerful tool for the high‐contrast visualization of internal textures such as streaks and lechatelierite in the tektite matrix due to the luminescence properties of the defect structures in the glassy network.</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="110256306"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="110256306"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 110256306; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=110256306]").text(description); $(".js-view-count[data-work-id=110256306]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 110256306; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='110256306']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=110256306]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":110256306,"title":"Cathodoluminescence of moldavites","internal_url":"https://www.academia.edu/110256306/Cathodoluminescence_of_moldavites","owner_id":38239714,"coauthors_can_edit":true,"owner":{"id":38239714,"first_name":"Jan-Michael","middle_initials":null,"last_name":"Lange","page_name":"janmichaellange","domain_name":"independent","created_at":"2015-11-12T22:17:29.378-08:00","display_name":"Jan-Michael Lange","url":"https://independent.academia.edu/janmichaellange"},"attachments":[]}, 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="110256231"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/110256231/The_Ries_impact_and_its_distal_effects_in_sediments_of_Central_Europe_A_review"><img alt="Research paper thumbnail of The Ries impact and its distal effects in sediments of Central Europe—A review" 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" rel="nofollow" href="https://www.academia.edu/110256231/The_Ries_impact_and_its_distal_effects_in_sediments_of_Central_Europe_A_review">The Ries impact and its distal effects in sediments of Central Europe—A review</a></div><div class="wp-workCard_item"><span>Meteoritics &amp; Planetary Science</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The Ries impact is the most important cosmic event in the younger geological history of Europe. 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 Ries impact is the most important cosmic event in the younger geological history of Europe. Its effects reach far beyond the area considered so far and are documented in manifold evidence. In this paper, the widely scattered reports in the literature are compiled and supported with investigations by the authors. Besides well‐known ejecta features like the Brockhorizont, Reuter&#39;s blocks, and moldavites, little known or forgotten indications, like a lechatelierite and β‐cristobalite occurrence in Bavaria and unusual sedimentation phenomena in northern Germany, are presented. The paleogeographic reconstruction shows that the Ries impact occurred on the southern side of the Neogene Central European mainland. Large parts of this erosional area were devastated by the impact. Pressure waves and thermal radiation had a lasting effect on the landscape within hundreds of kilometers around the impact site. Destruction of the vegetation cover by impact‐induced storms, wildfires, and hea...</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="110256231"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="110256231"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 110256231; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=110256231]").text(description); $(".js-view-count[data-work-id=110256231]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 110256231; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='110256231']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=110256231]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":110256231,"title":"The Ries impact and its distal effects in sediments of Central Europe—A review","internal_url":"https://www.academia.edu/110256231/The_Ries_impact_and_its_distal_effects_in_sediments_of_Central_Europe_A_review","owner_id":38239714,"coauthors_can_edit":true,"owner":{"id":38239714,"first_name":"Jan-Michael","middle_initials":null,"last_name":"Lange","page_name":"janmichaellange","domain_name":"independent","created_at":"2015-11-12T22:17:29.378-08:00","display_name":"Jan-Michael Lange","url":"https://independent.academia.edu/janmichaellange"},"attachments":[]}, 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="108138005"><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/108138005/Die_%C3%A4ltere_Geschichte_der_Radeberger_Lik%C3%B6rfabrik_Wilhelm_Richter"><img alt="Research paper thumbnail of Die ältere Geschichte der Radeberger Likörfabrik Wilhelm Richter" class="work-thumbnail" src="https://attachments.academia-assets.com/106601605/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/108138005/Die_%C3%A4ltere_Geschichte_der_Radeberger_Lik%C3%B6rfabrik_Wilhelm_Richter">Die ältere Geschichte der Radeberger Likörfabrik Wilhelm Richter</a></div><div class="wp-workCard_item"><span>Radeberger Blätter zur Stadtgeschichte</span><span>, 2020</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Über die Vorläufer, die Gründung und die ersten Jahrzehnte der Radeberger Likörfabrik Wilhelm Ric...</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">Über die Vorläufer, die Gründung und die ersten Jahrzehnte der Radeberger Likörfabrik Wilhelm Richter existieren einige Mythen und Widersprüchlichkeiten. Anhand der Quellenlage können jedoch zahlreiche Fixpunkte in der Geschichte dieses Betriebes aufgezeigt werden, die es ermöglichen, wichtige Etappen der Firmenentwicklung bis zum Zweiten Weltkrieg in den Grundzügen zu skizzieren.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="30c7bca83ff9da27cec3daa99d411206" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":106601605,"asset_id":108138005,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/106601605/download_file?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="108138005"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="108138005"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 108138005; 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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="99211327"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/99211327/The_Ries_impact_and_its_distal_effects_in_sediments_of_Central_Europe_A_review"><img alt="Research paper thumbnail of The Ries impact and its distal effects in sediments of Central Europe—A review" 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" rel="nofollow" href="https://www.academia.edu/99211327/The_Ries_impact_and_its_distal_effects_in_sediments_of_Central_Europe_A_review">The Ries impact and its distal effects in sediments of Central Europe—A review</a></div><div class="wp-workCard_item wp-workCard--coauthors"><span>by </span><span><a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/janmichaellange">Jan-Michael Lange</a> and <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/PeterSuhr">Peter Suhr</a></span></div><div class="wp-workCard_item"><span>Meteoritics and Planetary Science</span><span>, 2023</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The Ries impact is the most important cosmic event in the younger geological history of Europe. 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 Ries impact is the most important cosmic event in the younger geological history of Europe. Its effects reach far beyond the area considered so far and are documented in manifold evidence. In this paper, the widely scattered reports in the literature are compiled and supported with investigations by the authors. Besides well-known ejecta features like the Brockhorizont, Reuter's blocks, and moldavites, little known or forgotten indications, like a lechatelierite and β-cristobalite occurrence in Bavaria and unusual sedimentation phenomena in northern Germany, are presented. The paleogeographic reconstruction shows that the Ries impact occurred on the southern side of the Neogene Central European mainland. Large parts of this erosional area were devastated by the impact. Pressure waves and thermal radiation had a lasting effect on the landscape within hundreds of kilometers around the impact site. Destruction of the vegetation cover by impact-induced storms, wildfires, and heavy rainfall generated intense erosion. The adjacent sedimentation area to the north (Paleo-North Sea) experienced an increased and short-term supply of terrestrial debris to the marine environment. The stratigraphic coincidence of these exceptional sediments with the Ries event leads us to conclude that the distal effects of the impact are present here, which have so far received little or no attention in this context. The paper considers the different indications and sets them in a large-scale context.</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="99211327"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="99211327"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 99211327; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=99211327]").text(description); 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