{"id":953,"date":"2022-04-02T14:14:14","date_gmt":"2022-04-02T14:14:14","guid":{"rendered":"https:\/\/lyon.apbg.org\/?p=953"},"modified":"2026-02-10T08:46:34","modified_gmt":"2026-02-10T07:46:34","slug":"decouverte-de-lorigine-du-mont-brouilly","status":"publish","type":"post","link":"https:\/\/lyon.apbg.fr\/?p=953","title":{"rendered":"12\/06\/21 : D\u00e9couverte de l&rsquo;origine du Mont Brouilly"},"content":{"rendered":"\n<p>Comment expliquer l&rsquo;aspect en d\u00f4me du Mont Brouilly ?<\/p>\n\n\n\n<figure class=\"wp-block-image size-large\"><a href=\"https:\/\/lyon.apbg.fr\/wp-content\/uploads\/2026\/02\/9DD3430A-80B4-471B-AB2B-5FB3B6D52E03-scaled-1.jpeg\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"768\" src=\"https:\/\/lyon.apbg.fr\/wp-content\/uploads\/2026\/02\/9DD3430A-80B4-471B-AB2B-5FB3B6D52E03-scaled-1-1024x768.jpeg\" alt=\"\" class=\"wp-image-10\" srcset=\"https:\/\/lyon.apbg.fr\/wp-content\/uploads\/2026\/02\/9DD3430A-80B4-471B-AB2B-5FB3B6D52E03-scaled-1-1024x768.jpeg 1024w, https:\/\/lyon.apbg.fr\/wp-content\/uploads\/2026\/02\/9DD3430A-80B4-471B-AB2B-5FB3B6D52E03-scaled-1-300x225.jpeg 300w, https:\/\/lyon.apbg.fr\/wp-content\/uploads\/2026\/02\/9DD3430A-80B4-471B-AB2B-5FB3B6D52E03-scaled-1-768x576.jpeg 768w, https:\/\/lyon.apbg.fr\/wp-content\/uploads\/2026\/02\/9DD3430A-80B4-471B-AB2B-5FB3B6D52E03-scaled-1-1536x1152.jpeg 1536w, https:\/\/lyon.apbg.fr\/wp-content\/uploads\/2026\/02\/9DD3430A-80B4-471B-AB2B-5FB3B6D52E03-scaled-1-2048x1536.jpeg 2048w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/a><figcaption class=\"wp-element-caption\">Mont Brouilly<\/figcaption><\/figure>\n\n\n\n<p><\/p>\n\n\n\n<p>Hypoth\u00e8ses&#8230;.<br>Il existe diff\u00e9rents \u00e9v\u00e8nements g\u00e9ologiques \u00e0 l&rsquo;origine d&rsquo;un relief en forme de d\u00f4me, cela peut \u00eatre le r\u00e9sultat d&rsquo;un magmatisme volcanique, d&rsquo;une \u00e9rosion diff\u00e9rentielle des roches ou encore la cons\u00e9quence d&rsquo;une activit\u00e9 humaine&#8230;&nbsp;<br>Quelle hypoth\u00e8se est la plus vraisemblable pour vous?<\/p>\n\n\n\n<p>Pour r\u00e9pondre \u00e0 cette question,  nous avons organis\u00e9 une sortie de g\u00e9ologie sur le<strong>&nbsp;magmatisme arri\u00e8re-arc de la Br\u00e9venne-Beaujolais au Mont Brouilly <\/strong>avec Herv\u00e9 Bertrand,&nbsp;G\u00e9ologue Ecole-normale-superieure-de-Lyon le samedi 12 juin 2021.<\/p>\n\n\n\n<p>bilan <a href=\"https:\/\/www.youtube.com\/watch?v=yj0ryXDdmIQ\" data-type=\"URL\" data-id=\"https:\/\/www.youtube.com\/watch?v=yj0ryXDdmIQ\" target=\"_blank\" rel=\"noreferrer noopener\">video<\/a><br>Cette excursion se propose de rechercher les t\u00e9moins du magmatisme d\u2019arri\u00e8re-arc d\u00e9vonien sup\u00e9rieur (370-380 Ma) contemporain de la subduction N\u25caS de la Laurussia sous le Gondwana.&nbsp;Ces t\u00e9moins volcaniques (basaltes en pillow-lavas), hypovolcaniques (microdiorites), plutoniques (cumulats gabbro\u00efques) attestent d\u2019une cro\u00fbte oc\u00e9anique qui a ensuite \u00e9t\u00e9 d\u00e9membr\u00e9e lors de la collision varisque, au Carbonif\u00e8re. &nbsp;Lors de cette collision se mettent en place des granites, parmi lesquels le granite d\u2019Odenas-Fleurie (320-330 Ma).&nbsp;Ce dernier est intrusif au sein de microdiorites d\u00e9voniennes qui ont \u00e9t\u00e9 m\u00e9tamorphis\u00e9es au contact du granite, engendrant une aur\u00e9ole de corn\u00e9ennes \u00e0 l\u2019origine du Mont Brouilly actuel.<\/p>\n\n\n\n<p>N&rsquo;h\u00e9sitez pas \u00e0 consulter la pr\u00e9sentation dans cette <a href=\"https:\/\/storymaps.arcgis.com\/stories\/3ee67b0bdc0c465587336a6e4f5bb3cc\">story map<\/a><\/p>\n\n\n\n<p><br>Th\u00e8mes possibles pour les \u00e9l\u00e8ves&nbsp;:<\/p>\n\n\n\n<p>Sur la base d\u2019observations de terrain et cartographiques (France 1:1 000&nbsp;000\u00e8me, Beaujeu&nbsp;1&nbsp;:50&nbsp;000\u00e8me), cette excursion permet de discuter de diff\u00e9rents aspects, parmi lesquels&nbsp;:<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>enchainement subduction-collision dans une cha\u00eene de montagne (cha\u00eene varisque)<\/li>\n\n\n\n<li>recherche de t\u00e9moins \u00a0ophiolitiques disloqu\u00e9s (volcanisme oc\u00e9anique, hydrothermalisme, cumulats de chambre magmatique)<\/li>\n\n\n\n<li>chronologie relative entre un granite et un ensemble volcanique (m\u00e9tamorphisme de contact)<\/li>\n\n\n\n<li>g\u00e9ologie et substances utiles (carri\u00e8res, mat\u00e9riaux de construction)<\/li>\n\n\n\n<li>g\u00e9ologie et terroirs viticoles, une d\u00e9gustation est possible, l\u2019achat d\u2019une bouteille est\u00a0propos\u00e9\u00a0(les prix des Brouilly \/ C\u00f4tes de Brouilly sont entre 9 et 15 euros)<\/li>\n<\/ul>\n\n\n\n<p><a href=\"https:\/\/storymaps.arcgis.com\/stories\/3ee67b0bdc0c465587336a6e4f5bb3cc\">https:\/\/storymaps.arcgis.com\/stories\/3ee67b0bdc0c465587336a6e4f5bb3cc<\/a><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Comment expliquer l&rsquo;aspect en d\u00f4me du Mont Brouilly ? Hypoth\u00e8ses&#8230;.Il existe diff\u00e9rents \u00e9v\u00e8nements g\u00e9ologiques \u00e0 l&rsquo;origine d&rsquo;un relief en forme<\/p>\n","protected":false},"author":1,"featured_media":960,"comment_status":"closed","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"colormag_page_container_layout":"default_layout","colormag_page_sidebar_layout":"default_layout","footnotes":""},"categories":[6],"tags":[],"class_list":["post-953","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-sortie"],"_links":{"self":[{"href":"https:\/\/lyon.apbg.fr\/index.php?rest_route=\/wp\/v2\/posts\/953","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/lyon.apbg.fr\/index.php?rest_route=\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/lyon.apbg.fr\/index.php?rest_route=\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/lyon.apbg.fr\/index.php?rest_route=\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/lyon.apbg.fr\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=953"}],"version-history":[{"count":1,"href":"https:\/\/lyon.apbg.fr\/index.php?rest_route=\/wp\/v2\/posts\/953\/revisions"}],"predecessor-version":[{"id":1130,"href":"https:\/\/lyon.apbg.fr\/index.php?rest_route=\/wp\/v2\/posts\/953\/revisions\/1130"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/lyon.apbg.fr\/index.php?rest_route=\/"}],"wp:attachment":[{"href":"https:\/\/lyon.apbg.fr\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=953"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/lyon.apbg.fr\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=953"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/lyon.apbg.fr\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=953"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}