{"id":1398,"date":"2017-07-05T17:59:05","date_gmt":"2017-07-05T15:59:05","guid":{"rendered":"http:\/\/blog.unifr.ch\/tectonics\/?p=1398"},"modified":"2017-07-13T17:08:52","modified_gmt":"2017-07-13T15:08:52","slug":"1398-2","status":"publish","type":"post","link":"https:\/\/blog.unifr.ch\/tectonics\/1398-2\/","title":{"rendered":"Triassic Alpine D\u00e9collement &#8211; A Review"},"content":{"rendered":"<p>In the course of June 2017 our paper on our present knowledge of the Triassic evaporites and the foreland d\u00e9collements has been published in <strong>The Role of the Triassic Evaporites underneath the North Alpine Foreland , <\/strong><em>by Anna&nbsp;<\/em><em>Sommaruga, Jon Mosar, Marc Schori, Marius Gruber.&nbsp;<\/em>The paper covers different aspects of the Alpine foreland d\u00e9collement levels.&nbsp;<\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter wp-image-1402 size-full\" src=\"http:\/\/blog.unifr.ch\/tectonics\/wp-content\/uploads\/2017\/07\/Triassic-Decollement.png\" alt=\"\" width=\"761\" height=\"365\" srcset=\"https:\/\/blog.unifr.ch\/tectonics\/wp-content\/uploads\/2017\/07\/Triassic-Decollement.png 761w, https:\/\/blog.unifr.ch\/tectonics\/wp-content\/uploads\/2017\/07\/Triassic-Decollement-300x144.png 300w\" sizes=\"auto, (max-width: 761px) 100vw, 761px\" \/><\/p>\n<p>You can find more info on our blog pages on<\/p>\n<ul>\n<li class=\"entry-title\"><a href=\"http:\/\/blog.unifr.ch\/tectonics\/alpine-foreland-basal-detachment\/\"><em><strong>Alpine foreland basal detachment <\/strong><\/em><\/a><\/li>\n<li class=\"entry-title\"><a href=\"http:\/\/blog.unifr.ch\/tectonics\/basal-decollement-of-the-alpine-foreland\/\"><em><strong>Basal d\u00e9collement of the Alpine foreland<\/strong><\/em><\/a><\/li>\n<\/ul>\n<p>The paper is part&nbsp; of a book with of over 20 chapters on Permo-Triaassic salt provinces:&nbsp; <strong>Permo-Triassic Salt Provinces of Eu<\/strong><strong>rope, N<\/strong><strong>orth Africa and the Atlantic Margins. <\/strong>http:\/\/dx.doi.org\/10.1016\/B978-0-12-809417-4.00021-5, \u00a9 2017 Elsevier Inc.<\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"size-medium wp-image-1401 aligncenter\" src=\"http:\/\/blog.unifr.ch\/tectonics\/wp-content\/uploads\/2017\/07\/Salt-Book-AAPG-233x300.png\" alt=\"\" width=\"233\" height=\"300\" srcset=\"https:\/\/blog.unifr.ch\/tectonics\/wp-content\/uploads\/2017\/07\/Salt-Book-AAPG-233x300.png 233w, https:\/\/blog.unifr.ch\/tectonics\/wp-content\/uploads\/2017\/07\/Salt-Book-AAPG.png 612w\" sizes=\"auto, (max-width: 233px) 100vw, 233px\" \/><\/p>\n","protected":false},"excerpt":{"rendered":"<p>In the course of June 2017 our paper on our present knowledge of the Triassic evaporites and the foreland d\u00e9collements has been published in The Role of the Triassic Evaporites underneath the North Alpine Foreland , by Anna&nbsp;Sommaruga, Jon Mosar, Marc Schori, Marius Gruber.&nbsp;The paper covers different aspects of the Alpine foreland d\u00e9collement levels.&nbsp; You &hellip; <a href=\"https:\/\/blog.unifr.ch\/tectonics\/1398-2\/\" class=\"more-link\">Continue reading <span class=\"screen-reader-text\">Triassic Alpine D\u00e9collement &#8211; A Review<\/span> <span class=\"meta-nav\">&rarr;<\/span><\/a><\/p>\n","protected":false},"author":6,"featured_media":1410,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_s2mail":"yes","ngg_post_thumbnail":0,"footnotes":""},"categories":[1],"tags":[],"class_list":["post-1398","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-uncategorised"],"_links":{"self":[{"href":"https:\/\/blog.unifr.ch\/tectonics\/wp-json\/wp\/v2\/posts\/1398","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/blog.unifr.ch\/tectonics\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/blog.unifr.ch\/tectonics\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/blog.unifr.ch\/tectonics\/wp-json\/wp\/v2\/users\/6"}],"replies":[{"embeddable":true,"href":"https:\/\/blog.unifr.ch\/tectonics\/wp-json\/wp\/v2\/comments?post=1398"}],"version-history":[{"count":8,"href":"https:\/\/blog.unifr.ch\/tectonics\/wp-json\/wp\/v2\/posts\/1398\/revisions"}],"predecessor-version":[{"id":1417,"href":"https:\/\/blog.unifr.ch\/tectonics\/wp-json\/wp\/v2\/posts\/1398\/revisions\/1417"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/blog.unifr.ch\/tectonics\/wp-json\/wp\/v2\/media\/1410"}],"wp:attachment":[{"href":"https:\/\/blog.unifr.ch\/tectonics\/wp-json\/wp\/v2\/media?parent=1398"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/blog.unifr.ch\/tectonics\/wp-json\/wp\/v2\/categories?post=1398"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/blog.unifr.ch\/tectonics\/wp-json\/wp\/v2\/tags?post=1398"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}