{"id":3065,"date":"2022-01-31T22:49:53","date_gmt":"2022-01-31T21:49:53","guid":{"rendered":"https:\/\/lyon-geologie.univ-lyon1.fr\/?page_id=3065"},"modified":"2022-02-13T21:03:08","modified_gmt":"2022-02-13T20:03:08","slug":"l2-petrosed","status":"publish","type":"page","link":"https:\/\/lyongeologie.fr\/en\/l2-geosciences\/l2-petrosed\/","title":{"rendered":"L2 P\u00e9trographie s\u00e9dimentaire et Formations quaternaires"},"content":{"rendered":"<div data-elementor-type=\"wp-page\" data-elementor-id=\"3065\" class=\"elementor elementor-3065\">\n\t\t\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-5e50f57 elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"5e50f57\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-925ddb5\" data-id=\"925ddb5\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-d64734f elementor-widget elementor-widget-text-editor\" data-id=\"d64734f\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<h2>Sedimentary rocks and quaternary formations<\/h2>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-bb7acea elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"bb7acea\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-33 elementor-top-column elementor-element elementor-element-59475a6\" data-id=\"59475a6\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-ec15fc9 elementor-widget elementor-widget-text-editor\" data-id=\"ec15fc9\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<p><em>Credits: <\/em>6 ECTS<\/p><p><em>Semestre :<\/em> Printemps (S4)<\/p><p><em>Responsable: <a href=\"mailto:philippe.sorrel@univ-lyon1.fr\">Philippe SORREL<\/a><\/em><\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-6e3213c elementor-widget elementor-widget-image\" data-id=\"6e3213c\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"image.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<img decoding=\"async\" width=\"150\" height=\"150\" src=\"https:\/\/lyongeologie.fr\/wp-content\/uploads\/2022\/02\/philippe_sorrel-150x150.png\" class=\"attachment-thumbnail size-thumbnail wp-image-8913\" alt=\"\" srcset=\"https:\/\/lyongeologie.fr\/wp-content\/uploads\/2022\/02\/philippe_sorrel-150x150.png 150w, https:\/\/lyongeologie.fr\/wp-content\/uploads\/2022\/02\/philippe_sorrel-300x300.png 300w, https:\/\/lyongeologie.fr\/wp-content\/uploads\/2022\/02\/philippe_sorrel-1024x1024.png 1024w, https:\/\/lyongeologie.fr\/wp-content\/uploads\/2022\/02\/philippe_sorrel-768x767.png 768w, https:\/\/lyongeologie.fr\/wp-content\/uploads\/2022\/02\/philippe_sorrel.png 1030w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/>\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-81b4e3f elementor-align-center elementor-widget elementor-widget-button\" data-id=\"81b4e3f\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"button.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<div class=\"elementor-button-wrapper\">\n\t\t\t\t\t<a class=\"elementor-button elementor-button-link elementor-size-sm\" href=\"https:\/\/lyon-geologie.univ-lyon1.fr\/l2-geosciences\/#l2_tc\">\n\t\t\t\t\t\t<span class=\"elementor-button-content-wrapper\">\n\t\t\t\t\t\t\t\t\t<span class=\"elementor-button-text\">Back to the previous page<\/span>\n\t\t\t\t\t<\/span>\n\t\t\t\t\t<\/a>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t<div class=\"elementor-column elementor-col-66 elementor-top-column elementor-element elementor-element-f777f02\" data-id=\"f777f02\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-54d4e9e elementor-widget elementor-widget-text-editor\" data-id=\"54d4e9e\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<p>L\u2019objectif de cette UE est de vous fournir <strong>des bases solides en s\u00e9dimentologie<\/strong> et p\u00e9trographie s\u00e9dimentaire (analyse du microfaci\u00e8s). Il s\u2019agira de <strong>caract\u00e9riser les principaux environnements de d\u00e9p\u00f4t<\/strong>, depuis l\u2019\u00e9chelle macroscopique \u00e0 l\u2019\u00e9chelle microscopique, ainsi que leur mode de formation en relation avec les <strong>contextes environnementaux<\/strong> dans lesquels on les trouve.<\/p><p>Cette UE sera aussi l\u2019opportunit\u00e9 de traiter diverses probl\u00e9matiques inh\u00e9rentes aux formations s\u00e9dimentaires quaternaires, en relation avec les <strong>variations climatiques du Quaternaire<\/strong> dont la s\u00e9dimentologie p\u00e9riglaciaire en domaine continental, les terrasses marines interglaciaires et leur potentiel de reconstruction des pal\u00e9o-niveaux marins \/ contexte tectonique r\u00e9gional, la dynamique des versants en contexte glaciaire\/interglaciaire ainsi que la s\u00e9dimentologie oc\u00e9anique.<\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-b28b457 elementor-widget elementor-widget-image\" data-id=\"b28b457\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"image.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<img fetchpriority=\"high\" decoding=\"async\" width=\"1024\" height=\"593\" src=\"https:\/\/lyongeologie.fr\/wp-content\/uploads\/2022\/01\/L2_petrosed-1024x593.jpg\" class=\"attachment-large size-large wp-image-3079\" alt=\"Exemple d\u2019environnements s\u00e9dimentaires \u00e9tudi\u00e9s (avec analyse p\u00e9trographique du microfaci\u00e8s). Exemple de formations s\u00e9dimentaires quaternaires et de probl\u00e9matiques abord\u00e9es (ex : dynamique des versants au cours d\u2019un cycle climatique quaternaire)\" srcset=\"https:\/\/lyongeologie.fr\/wp-content\/uploads\/2022\/01\/L2_petrosed-1024x593.jpg 1024w, https:\/\/lyongeologie.fr\/wp-content\/uploads\/2022\/01\/L2_petrosed-300x174.jpg 300w, https:\/\/lyongeologie.fr\/wp-content\/uploads\/2022\/01\/L2_petrosed-768x444.jpg 768w, https:\/\/lyongeologie.fr\/wp-content\/uploads\/2022\/01\/L2_petrosed.jpg 1144w\" sizes=\"(max-width: 1024px) 100vw, 1024px\" \/>\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-e2f46dd elementor-widget elementor-widget-text-editor\" data-id=\"e2f46dd\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<p>Cette UE comporte 20h de CM, 12h de TD et 28h de TP incluant <strong>plusieurs sorties sur le terrain<\/strong> dans des formations s\u00e9dimentaires quaternaires (s\u00e9dimentologie et g\u00e9omorphologie glaciaire des environs de Lyon, dont un atelier dans une carri\u00e8re de granulats).<\/p><p>Elle se prolonge en L3 G\u00e9oS par les UE \u00ab\u00a0<a href=\"https:\/\/lyon-geologie.univ-lyon1.fr\/en\/l3-geosciences\/l3g_petrosed\/\">Sedimentary facies and processes<\/a>\u00ab\u00a0, \u00ab\u00a0<a href=\"https:\/\/lyon-geologie.univ-lyon1.fr\/en\/l3-geosciences\/l3g_6terrain_sedim\/\">\u00e9cole de terrain: s\u00e9dimentologie<\/a>\u00a0\u00bb et \u00ab\u00a0<a href=\"https:\/\/lyon-geologie.univ-lyon1.fr\/en\/l3-geosciences\/l3g_bassins\/\">Sedimentary basins<\/a>\u00ab\u00a0.<\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-655f7a9 elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"655f7a9\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-922acb4\" data-id=\"922acb4\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap\">\n\t\t\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<\/div>","protected":false},"excerpt":{"rendered":"<p>P\u00e9trographie S\u00e9dimentaire et Formations Quaternaires Cr\u00e9dits : 6 ECTS Semestre : Printemps (S4) Responsable: Philippe SORREL Retour \u00e0 la liste des UEs L\u2019objectif de cette UE est de vous fournir des bases solides en s\u00e9dimentologie et p\u00e9trographie s\u00e9dimentaire (analyse du microfaci\u00e8s). Il s\u2019agira de caract\u00e9riser les principaux environnements de d\u00e9p\u00f4t, depuis l\u2019\u00e9chelle macroscopique \u00e0 l\u2019\u00e9chelle [&hellip;]<\/p>\n","protected":false},"author":3,"featured_media":0,"parent":479,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"site-sidebar-layout":"no-sidebar","site-content-layout":"page-builder","ast-site-content-layout":"default","site-content-style":"default","site-sidebar-style":"default","ast-global-header-display":"","ast-banner-title-visibility":"","ast-main-header-display":"","ast-hfb-above-header-display":"","ast-hfb-below-header-display":"","ast-hfb-mobile-header-display":"","site-post-title":"disabled","ast-breadcrumbs-content":"","ast-featured-img":"disabled","footer-sml-layout":"","ast-disable-related-posts":"","theme-transparent-header-meta":"","adv-header-id-meta":"","stick-header-meta":"","header-above-stick-meta":"","header-main-stick-meta":"","header-below-stick-meta":"","astra-migrate-meta-layouts":"default","ast-page-background-enabled":"default","ast-page-background-meta":{"desktop":{"background-color":"var(--ast-global-color-4)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"tablet":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"mobile":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""}},"ast-content-background-meta":{"desktop":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"tablet":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"mobile":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""}},"footnotes":""},"class_list":["post-3065","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/lyongeologie.fr\/en\/wp-json\/wp\/v2\/pages\/3065","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/lyongeologie.fr\/en\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/lyongeologie.fr\/en\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/lyongeologie.fr\/en\/wp-json\/wp\/v2\/users\/3"}],"replies":[{"embeddable":true,"href":"https:\/\/lyongeologie.fr\/en\/wp-json\/wp\/v2\/comments?post=3065"}],"version-history":[{"count":39,"href":"https:\/\/lyongeologie.fr\/en\/wp-json\/wp\/v2\/pages\/3065\/revisions"}],"predecessor-version":[{"id":13227,"href":"https:\/\/lyongeologie.fr\/en\/wp-json\/wp\/v2\/pages\/3065\/revisions\/13227"}],"up":[{"embeddable":true,"href":"https:\/\/lyongeologie.fr\/en\/wp-json\/wp\/v2\/pages\/479"}],"wp:attachment":[{"href":"https:\/\/lyongeologie.fr\/en\/wp-json\/wp\/v2\/media?parent=3065"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}