{"id":352,"date":"2010-09-06T11:02:50","date_gmt":"2010-09-06T09:02:50","guid":{"rendered":"http:\/\/wp.unil.ch\/sciencesaucarre\/?p=352"},"modified":"2010-11-09T15:21:59","modified_gmt":"2010-11-09T14:21:59","slug":"epard-jean-luc","status":"publish","type":"post","link":"https:\/\/wp.unil.ch\/sciencesaucarre\/epard-jean-luc\/","title":{"rendered":"Epard Jean-Luc"},"content":{"rendered":"<p><strong>Professeur associ\u00e9<br \/>\n<\/strong><\/p>\n<p><em>Facult\u00e9 des g\u00e9osciences et de l&rsquo;environnement &#8211; UNIL<\/em><\/p>\n<p><em><!--more-->G\u00e9ologie et Pal\u00e9ontologie<br \/>\n<a href=\"mailto:jean-luc.epard@unil.ch\"> jean-luc.epard@unil.ch<\/a><br \/>\nT\u00e9l. <\/em>+41 21 692 43 66<\/p>\n<h4>Langues d&rsquo;enseignement<\/h4>\n<p>Fran\u00e7ais<\/p>\n<h4>Th\u00e8mes de pr\u00e9dilection<\/h4>\n<p>Formation des cha\u00eenes de montagnes, Alpes et Himalaya.<br \/>\nAnalyse de la structure de la roche acquise par la d\u00e9formation, formation des plis et des fractures.<br \/>\nCartographie g\u00e9ologique.<\/p>\n<h4>Comp\u00e9tences \u00e9largies<\/h4>\n<p>G\u00e9ologie r\u00e9gionale de Suisse occidentale, g\u00e9ologie des Alpes; g\u00e9ologie de l&rsquo;Himalaya Indien. G\u00e9ologie structurale.<br \/>\nUtilisation de la t\u00e9l\u00e9d\u00e9tection pour la cartographie g\u00e9ologique et la tectonique.<br \/>\nCours et travaux pratiques de g\u00e9ologie g\u00e9n\u00e9rale pour biologistes.<\/p>\n<h4>Th\u00e8mes de recherche sp\u00e9cifique<\/h4>\n<p>Plis de d\u00e9collement et fracturation associ\u00e9e (Jura, Appalaches, Rocheuses).<br \/>\nStructure et stratigraphie des nappes helv\u00e9tiques de Suisse occidentales.<br \/>\nStructure et lithostratigraphie des nappes Simplo-Tessinoises (Pennique inf\u00e9rieur, Tessin, Italie).<br \/>\nStructure, cin\u00e9matique et exhumation de nappes contenant des \u00e9clogites (Himalaya, Inde).<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Professeur associ\u00e9 Facult\u00e9 des g\u00e9osciences et de l&rsquo;environnement &#8211; UNIL<\/p>\n","protected":false},"author":236,"featured_media":0,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_seopress_robots_primary_cat":"","_seopress_titles_title":"","_seopress_titles_desc":"","_seopress_robots_index":"","footnotes":""},"categories":[39],"tags":[6275,6279,6278,6277,6276],"class_list":{"0":"post-352","1":"post","2":"type-post","3":"status-publish","4":"format-standard","6":"category-geosciences","7":"tag-alpes","8":"tag-cartographie-geologique","9":"tag-chaines-de-montagnes","10":"tag-geologie-structurale","11":"tag-himalaya"},"_links":{"self":[{"href":"https:\/\/wp.unil.ch\/sciencesaucarre\/wp-json\/wp\/v2\/posts\/352","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/wp.unil.ch\/sciencesaucarre\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/wp.unil.ch\/sciencesaucarre\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/wp.unil.ch\/sciencesaucarre\/wp-json\/wp\/v2\/users\/236"}],"replies":[{"embeddable":true,"href":"https:\/\/wp.unil.ch\/sciencesaucarre\/wp-json\/wp\/v2\/comments?post=352"}],"version-history":[{"count":0,"href":"https:\/\/wp.unil.ch\/sciencesaucarre\/wp-json\/wp\/v2\/posts\/352\/revisions"}],"wp:attachment":[{"href":"https:\/\/wp.unil.ch\/sciencesaucarre\/wp-json\/wp\/v2\/media?parent=352"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/wp.unil.ch\/sciencesaucarre\/wp-json\/wp\/v2\/categories?post=352"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/wp.unil.ch\/sciencesaucarre\/wp-json\/wp\/v2\/tags?post=352"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}