{"id":6091,"date":"2020-08-22T09:40:42","date_gmt":"2020-08-22T09:40:42","guid":{"rendered":"https:\/\/blogs.futura-sciences.com\/bardintzeff\/?p=6091"},"modified":"2020-08-22T09:42:19","modified_gmt":"2020-08-22T09:42:19","slug":"le-pli-faille-de-sassenage-alpes","status":"publish","type":"post","link":"https:\/\/blogs.futura-sciences.com\/bardintzeff\/2020\/08\/22\/le-pli-faille-de-sassenage-alpes\/","title":{"rendered":"Le pli-faille de Sassenage, Alpes"},"content":{"rendered":"<p>Le pli-faille de Sassenage est une c\u00e9l\u00e8bre structure tectonique dans les Alpes (massif subalpin du Vercors). Le pli, couch\u00e9 vers l\u2019ouest, s\u2019est rompu (faille) dans son flanc inf\u00e9rieur. On le voit nettement dans la vall\u00e9e fluvio-glaciaire (cluse) de l\u2019Is\u00e8re.<\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"alignnone size-medium wp-image-6094\" src=\"https:\/\/blogs.futura-sciences.com\/bardintzeff\/wp-content\/uploads\/sites\/3\/2020\/08\/Bardintzeff.2020.07.30.Saint_Egreve2.pli_faille_Sassenage.low_.s-450x338.jpg\" alt=\"\" width=\"450\" height=\"338\" srcset=\"https:\/\/blogs.futura-sciences.com\/bardintzeff\/wp-content\/uploads\/sites\/3\/2020\/08\/Bardintzeff.2020.07.30.Saint_Egreve2.pli_faille_Sassenage.low_.s-450x338.jpg 450w, https:\/\/blogs.futura-sciences.com\/bardintzeff\/wp-content\/uploads\/sites\/3\/2020\/08\/Bardintzeff.2020.07.30.Saint_Egreve2.pli_faille_Sassenage.low_.s-1024x768.jpg 1024w, https:\/\/blogs.futura-sciences.com\/bardintzeff\/wp-content\/uploads\/sites\/3\/2020\/08\/Bardintzeff.2020.07.30.Saint_Egreve2.pli_faille_Sassenage.low_.s-768x576.jpg 768w, https:\/\/blogs.futura-sciences.com\/bardintzeff\/wp-content\/uploads\/sites\/3\/2020\/08\/Bardintzeff.2020.07.30.Saint_Egreve2.pli_faille_Sassenage.low_.s.jpg 1417w\" sizes=\"auto, (max-width: 450px) 100vw, 450px\" \/><\/p>\n<p>Le pli-faille de Sassenage (38360), vu de Saint-\u00c9gr\u00e8ve (38120), le matin (\u00a9 J.M. Bardintzeff).<\/p>\n<p><!--more--><\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"alignnone size-medium wp-image-6096\" src=\"https:\/\/blogs.futura-sciences.com\/bardintzeff\/wp-content\/uploads\/sites\/3\/2020\/08\/Bardintzeff.2020.07.29.Saint_Egreve.pli_faille_Sassenage.low_.s-450x338.jpg\" alt=\"\" width=\"450\" height=\"338\" srcset=\"https:\/\/blogs.futura-sciences.com\/bardintzeff\/wp-content\/uploads\/sites\/3\/2020\/08\/Bardintzeff.2020.07.29.Saint_Egreve.pli_faille_Sassenage.low_.s-450x338.jpg 450w, https:\/\/blogs.futura-sciences.com\/bardintzeff\/wp-content\/uploads\/sites\/3\/2020\/08\/Bardintzeff.2020.07.29.Saint_Egreve.pli_faille_Sassenage.low_.s-1024x768.jpg 1024w, https:\/\/blogs.futura-sciences.com\/bardintzeff\/wp-content\/uploads\/sites\/3\/2020\/08\/Bardintzeff.2020.07.29.Saint_Egreve.pli_faille_Sassenage.low_.s-768x576.jpg 768w, https:\/\/blogs.futura-sciences.com\/bardintzeff\/wp-content\/uploads\/sites\/3\/2020\/08\/Bardintzeff.2020.07.29.Saint_Egreve.pli_faille_Sassenage.low_.s.jpg 1417w\" sizes=\"auto, (max-width: 450px) 100vw, 450px\" \/><\/p>\n<p>Le pli-faille de Sassenage (38360), vu de Saint-\u00c9gr\u00e8ve (38120), en fin d\u2019apr\u00e8s-midi (\u00a9 J.M. Bardintzeff).<\/p>\n<!-- AddThis Advanced Settings generic via filter on the_content --><!-- AddThis Share Buttons generic via filter on the_content -->","protected":false},"excerpt":{"rendered":"<p>Le pli-faille de Sassenage est une c\u00e9l\u00e8bre structure tectonique dans les Alpes (massif subalpin du Vercors). Le pli, couch\u00e9 vers l\u2019ouest, s\u2019est rompu (faille) dans son flanc inf\u00e9rieur. On le voit nettement dans la vall\u00e9e fluvio-glaciaire (cluse) de l\u2019Is\u00e8re. Le pli-faille de Sassenage (38360), vu de Saint-\u00c9gr\u00e8ve (38120), le matin (\u00a9 J.M. Bardintzeff).<!-- AddThis Advanced Settings generic via filter on get_the_excerpt --><!-- AddThis Share Buttons generic via filter on get_the_excerpt --><\/p>\n","protected":false},"author":3,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":"","_links_to":"","_links_to_target":""},"categories":[8],"tags":[79,684,312,686,2116,688,2117,1931,692],"class_list":["post-6091","post","type-post","status-publish","format-standard","hentry","category-voyages","tag-alpes","tag-cluse","tag-isere","tag-pli","tag-pli-faille","tag-saint-egreve","tag-sassenage","tag-tectonique","tag-vercors"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v24.1 - https:\/\/yoast.com\/wordpress\/plugins\/seo\/ -->\n<title>Le pli-faille de Sassenage, Alpes, par Jacques-Marie Bardintzeff<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/blogs.futura-sciences.com\/bardintzeff\/2020\/08\/22\/le-pli-faille-de-sassenage-alpes\/\" \/>\n<meta property=\"og:locale\" content=\"fr_FR\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Le pli-faille de Sassenage, Alpes, par Jacques-Marie Bardintzeff\" \/>\n<meta property=\"og:description\" content=\"Le pli-faille de Sassenage est une c\u00e9l\u00e8bre structure tectonique dans les Alpes (massif subalpin du Vercors). Le pli, couch\u00e9 vers l\u2019ouest, s\u2019est rompu (faille) dans son flanc inf\u00e9rieur. On le voit nettement dans la vall\u00e9e fluvio-glaciaire (cluse) de l\u2019Is\u00e8re. Le pli-faille de Sassenage (38360), vu de Saint-\u00c9gr\u00e8ve (38120), le matin (\u00a9 J.M. 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