{"id":508,"date":"2016-11-22T15:39:35","date_gmt":"2016-11-22T14:39:35","guid":{"rendered":"http:\/\/blog.unifr.ch\/tectonics\/?page_id=508"},"modified":"2016-12-14T10:38:08","modified_gmt":"2016-12-14T09:38:08","slug":"3d-images-of-eclepens-quarry","status":"publish","type":"page","link":"https:\/\/blog.unifr.ch\/tectonics\/3d-images-of-eclepens-quarry\/","title":{"rendered":"3D images of Eclepens quarry"},"content":{"rendered":"<p>The Eclepens\/Mormont quarry is located at the SE tip of the dextral Mormont tear fault. This fault show a regional Riedel zone geometry and strong local anisotropy.<\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter wp-image-1060 size-large\" src=\"http:\/\/blog.unifr.ch\/tectonics\/wp-content\/uploads\/2016\/11\/Carri\u00e8re-Mormont-Eclepens-1024x235.jpg\" alt=\"SAMSUNG CSC\" width=\"604\" height=\"139\" srcset=\"https:\/\/blog.unifr.ch\/tectonics\/wp-content\/uploads\/2016\/11\/Carri\u00e8re-Mormont-Eclepens-1024x235.jpg 1024w, https:\/\/blog.unifr.ch\/tectonics\/wp-content\/uploads\/2016\/11\/Carri\u00e8re-Mormont-Eclepens-300x69.jpg 300w, https:\/\/blog.unifr.ch\/tectonics\/wp-content\/uploads\/2016\/11\/Carri\u00e8re-Mormont-Eclepens-768x176.jpg 768w\" sizes=\"auto, (max-width: 604px) 100vw, 604px\" \/><\/p>\n<p>During our recent work on tear faults and fault zone anatomy in the Eclepens-Mormont quarry we have used a drone to make a 3D rendering of the quarry:&nbsp;<\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-876 size-large aligncenter\" src=\"http:\/\/blog.unifr.ch\/tectonics\/wp-content\/uploads\/2016\/11\/quarry-eclepens-1024x622.jpg\" alt=\"quarry-eclepens\" width=\"604\" height=\"367\" srcset=\"https:\/\/blog.unifr.ch\/tectonics\/wp-content\/uploads\/2016\/11\/quarry-eclepens-1024x622.jpg 1024w, https:\/\/blog.unifr.ch\/tectonics\/wp-content\/uploads\/2016\/11\/quarry-eclepens-300x182.jpg 300w, https:\/\/blog.unifr.ch\/tectonics\/wp-content\/uploads\/2016\/11\/quarry-eclepens-768x466.jpg 768w, https:\/\/blog.unifr.ch\/tectonics\/wp-content\/uploads\/2016\/11\/quarry-eclepens.jpg 1313w\" sizes=\"auto, (max-width: 604px) 100vw, 604px\" \/><\/p>\n<p>click on picture for animation of drone flight.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>The Eclepens\/Mormont quarry is located at the SE tip of the dextral Mormont tear fault. This fault show a regional Riedel zone geometry and strong local anisotropy. During our recent work on tear faults and fault zone anatomy in the Eclepens-Mormont quarry we have used a drone to make a 3D rendering of the quarry:&nbsp; &hellip; <a href=\"https:\/\/blog.unifr.ch\/tectonics\/3d-images-of-eclepens-quarry\/\" class=\"more-link\">Continue reading <span class=\"screen-reader-text\">3D images of Eclepens quarry<\/span> <span class=\"meta-nav\">&rarr;<\/span><\/a><\/p>\n","protected":false},"author":2,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_s2mail":"","ngg_post_thumbnail":0,"footnotes":""},"class_list":["post-508","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/blog.unifr.ch\/tectonics\/wp-json\/wp\/v2\/pages\/508","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/blog.unifr.ch\/tectonics\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/blog.unifr.ch\/tectonics\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/blog.unifr.ch\/tectonics\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/blog.unifr.ch\/tectonics\/wp-json\/wp\/v2\/comments?post=508"}],"version-history":[{"count":6,"href":"https:\/\/blog.unifr.ch\/tectonics\/wp-json\/wp\/v2\/pages\/508\/revisions"}],"predecessor-version":[{"id":1061,"href":"https:\/\/blog.unifr.ch\/tectonics\/wp-json\/wp\/v2\/pages\/508\/revisions\/1061"}],"wp:attachment":[{"href":"https:\/\/blog.unifr.ch\/tectonics\/wp-json\/wp\/v2\/media?parent=508"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}