{"id":510,"date":"2016-11-22T15:39:48","date_gmt":"2016-11-22T14:39:48","guid":{"rendered":"http:\/\/blog.unifr.ch\/tectonics\/?page_id=510"},"modified":"2016-12-02T15:31:23","modified_gmt":"2016-12-02T14:31:23","slug":"fracturing-the-jura","status":"publish","type":"page","link":"https:\/\/blog.unifr.ch\/tectonics\/fracturing-the-jura\/","title":{"rendered":"Fracturing the Jura"},"content":{"rendered":"<p>Recent work on fraqctures in th Central Jura Mountains by two MAster students (Thibaud Rey (images) and Ahtos Tad\u00e9) have shown the complex fault pattern and its link to the regional tectonics as well as the protential reactivation in a changing stress field.<\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-873 aligncenter\" src=\"http:\/\/blog.unifr.ch\/tectonics\/wp-content\/uploads\/2016\/11\/Fig.53-891x1024.jpg\" alt=\"fig-53\" width=\"500\" height=\"575\" srcset=\"https:\/\/blog.unifr.ch\/tectonics\/wp-content\/uploads\/2016\/11\/Fig.53-891x1024.jpg 891w, https:\/\/blog.unifr.ch\/tectonics\/wp-content\/uploads\/2016\/11\/Fig.53-261x300.jpg 261w, https:\/\/blog.unifr.ch\/tectonics\/wp-content\/uploads\/2016\/11\/Fig.53-768x883.jpg 768w\" sizes=\"auto, (max-width: 500px) 100vw, 500px\" \/><\/p>\n<p>The main fault directions are often not those suspected from field geology and are revealed by investigating the digital elevation model:<\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter wp-image-872\" src=\"http:\/\/blog.unifr.ch\/tectonics\/wp-content\/uploads\/2016\/11\/Fig.74-1024x553.jpg\" alt=\"fig-74\" width=\"400\" height=\"216\" srcset=\"https:\/\/blog.unifr.ch\/tectonics\/wp-content\/uploads\/2016\/11\/Fig.74-1024x553.jpg 1024w, https:\/\/blog.unifr.ch\/tectonics\/wp-content\/uploads\/2016\/11\/Fig.74-300x162.jpg 300w, https:\/\/blog.unifr.ch\/tectonics\/wp-content\/uploads\/2016\/11\/Fig.74-768x415.jpg 768w\" sizes=\"auto, (max-width: 400px) 100vw, 400px\" \/><\/p>\n<p>The most difficult part in the interpretation is attributing the numerous and apparently randomly oriented faults to a distinct structural context and\/or a reactivation:<\/p>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Recent work on fraqctures in th Central Jura Mountains by two MAster students (Thibaud Rey (images) and Ahtos Tad\u00e9) have shown the complex fault pattern and its link to the regional tectonics as well as the protential reactivation in a changing stress field. The main fault directions are often not those suspected from field geology &hellip; <a href=\"https:\/\/blog.unifr.ch\/tectonics\/fracturing-the-jura\/\" class=\"more-link\">Continue reading <span class=\"screen-reader-text\">Fracturing the Jura<\/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-510","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/blog.unifr.ch\/tectonics\/wp-json\/wp\/v2\/pages\/510","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=510"}],"version-history":[{"count":5,"href":"https:\/\/blog.unifr.ch\/tectonics\/wp-json\/wp\/v2\/pages\/510\/revisions"}],"predecessor-version":[{"id":878,"href":"https:\/\/blog.unifr.ch\/tectonics\/wp-json\/wp\/v2\/pages\/510\/revisions\/878"}],"wp:attachment":[{"href":"https:\/\/blog.unifr.ch\/tectonics\/wp-json\/wp\/v2\/media?parent=510"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}