{"id":2150,"date":"2024-02-25T10:46:41","date_gmt":"2024-02-25T09:46:41","guid":{"rendered":"https:\/\/svt-dalaine.fr\/svt\/?page_id=2150"},"modified":"2026-02-17T11:31:07","modified_gmt":"2026-02-17T10:31:07","slug":"st-d-1-la-rheologie-de-la-lithosphere","status":"publish","type":"page","link":"https:\/\/svt-dalaine.fr\/svt\/st-d-1-la-rheologie-de-la-lithosphere\/","title":{"rendered":"ST-D-1 La rh\u00e9ologie de la lithosph\u00e8re"},"content":{"rendered":"\t\t<div data-elementor-type=\"wp-page\" data-elementor-id=\"2150\" class=\"elementor elementor-2150\">\n\t\t\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-6733ffa elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"6733ffa\" data-element_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-1cfd472\" data-id=\"1cfd472\" data-element_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-34a2130 elementor-widget elementor-widget-image\" data-id=\"34a2130\" data-element_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<img fetchpriority=\"high\" decoding=\"async\" width=\"640\" height=\"480\" src=\"https:\/\/svt-dalaine.fr\/svt\/wp-content\/uploads\/2024\/02\/L-tectonique1-768x576.jpg\" class=\"attachment-medium_large size-medium_large wp-image-2153\" alt=\"\" srcset=\"https:\/\/svt-dalaine.fr\/svt\/wp-content\/uploads\/2024\/02\/L-tectonique1-768x576.jpg 768w, https:\/\/svt-dalaine.fr\/svt\/wp-content\/uploads\/2024\/02\/L-tectonique1-300x225.jpg 300w, https:\/\/svt-dalaine.fr\/svt\/wp-content\/uploads\/2024\/02\/L-tectonique1-1024x768.jpg 1024w, https:\/\/svt-dalaine.fr\/svt\/wp-content\/uploads\/2024\/02\/L-tectonique1-1536x1152.jpg 1536w, https:\/\/svt-dalaine.fr\/svt\/wp-content\/uploads\/2024\/02\/L-tectonique1-360x270.jpg 360w, https:\/\/svt-dalaine.fr\/svt\/wp-content\/uploads\/2024\/02\/L-tectonique1.jpg 2048w\" sizes=\"(max-width: 640px) 100vw, 640px\" \/>\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\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-62d59e1 elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"62d59e1\" data-element_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-b09c245\" data-id=\"b09c245\" data-element_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-580137f elementor-widget elementor-widget-text-editor\" data-id=\"580137f\" data-element_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<p>Extrait du B.O.<\/p><p>Les mat\u00e9riaux lithosph\u00e9riques se d\u00e9forment sous l\u2019effet de contraintes : la d\u00e9formation est r\u00e9versible ou irr\u00e9versible.<\/p><p>La d\u00e9formation finie peut se d\u00e9composer en \u00e9tapes (ou incr\u00e9ments) de deux types comportant ou non une part de rotation. Le cisaillement est alors pur ou simple. Les propri\u00e9t\u00e9s m\u00e9caniques des roches d\u00e9pendent de leur min\u00e9ralogie, des conditions pression\/temp\u00e9rature et de la pr\u00e9sence de fluides ainsi que de la vitesse de d\u00e9formation.<\/p><p>Ces propri\u00e9t\u00e9s m\u00e9caniques m\u00e8nent \u00e0 la d\u00e9finition thermom\u00e9canique de la lithosph\u00e8re abord\u00e9e pr\u00e9c\u00e9demment.<\/p><p>Le comportement global de la lithosph\u00e8re est d\u00e9termin\u00e9 par son enveloppe rh\u00e9ologique, mais ce mod\u00e8le statique est questionn\u00e9 par des observations de terrain ainsi que par des donn\u00e9es g\u00e9ophysiques.<\/p>\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-9b5d658 elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"9b5d658\" data-element_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-4638ba4\" data-id=\"4638ba4\" data-element_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-1993d10 elementor-widget elementor-widget-text-editor\" data-id=\"1993d10\" data-element_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<p>TD de rh\u00e9ologie \u00e0 r\u00e9aliser en autonomie avant la s\u00e9ance du mercredi. Bon voyage!<\/p>\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-81b13f2 elementor-widget elementor-widget-text-editor\" data-id=\"81b13f2\" data-element_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<p><iframe class=\"wp-embedded-content\" sandbox=\"allow-scripts\" security=\"restricted\" title=\"TD-ST-D-1-Rh\u00e9ologie\" frameborder='0' width='1200' height='675' src='https:\/\/view.genial.ly\/653ce79be081880010291311#?secret=9bX9kaR442' data-secret='9bX9kaR442' scrolling='yes'><\/iframe><\/p>\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<\/div>\n\t\t","protected":false},"excerpt":{"rendered":"<p>Extrait du B.O. Les mat\u00e9riaux lithosph\u00e9riques se d\u00e9forment sous l\u2019effet de contraintes : la d\u00e9formation est r\u00e9versible ou irr\u00e9versible. La d\u00e9formation finie peut se d\u00e9composer en \u00e9tapes (ou incr\u00e9ments) de deux types comportant ou non une part de rotation. Le&hellip;&nbsp;<a href=\"https:\/\/svt-dalaine.fr\/svt\/st-d-1-la-rheologie-de-la-lithosphere\/\" class=\"more-link\">Lire la suite<\/a><\/p>\n","protected":false},"author":1,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"categories":[],"tags":[],"class_list":["post-2150","page","type-page","status-publish","hentry"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v21.9.1 - https:\/\/yoast.com\/wordpress\/plugins\/seo\/ -->\n<title>ST-D-1 La rh\u00e9ologie de la lithosph\u00e8re - Bienvenue sur le site de Sciences de la Vie et de la Terre<\/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:\/\/svt-dalaine.fr\/svt\/st-d-1-la-rheologie-de-la-lithosphere\/\" \/>\n<meta property=\"og:locale\" content=\"fr_FR\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"ST-D-1 La rh\u00e9ologie de la lithosph\u00e8re - Bienvenue sur le site de Sciences de la Vie et de la Terre\" \/>\n<meta property=\"og:description\" content=\"Extrait du B.O. Les mat\u00e9riaux lithosph\u00e9riques se d\u00e9forment sous l\u2019effet de contraintes : la d\u00e9formation est r\u00e9versible ou irr\u00e9versible. La d\u00e9formation finie peut se d\u00e9composer en \u00e9tapes (ou incr\u00e9ments) de deux types comportant ou non une part de rotation. Le&hellip;&nbsp;Lire la suite\" \/>\n<meta property=\"og:url\" content=\"https:\/\/svt-dalaine.fr\/svt\/st-d-1-la-rheologie-de-la-lithosphere\/\" \/>\n<meta property=\"og:site_name\" content=\"Bienvenue sur le site de Sciences de la Vie et de la Terre\" \/>\n<meta property=\"article:modified_time\" content=\"2026-02-17T10:31:07+00:00\" \/>\n<meta property=\"og:image\" content=\"https:\/\/svt-dalaine.fr\/svt\/wp-content\/uploads\/2024\/02\/L-tectonique1-768x576.jpg\" \/>\n<meta name=\"twitter:card\" content=\"summary_large_image\" \/>\n<meta name=\"twitter:label1\" content=\"Dur\u00e9e de lecture estim\u00e9e\" \/>\n\t<meta name=\"twitter:data1\" content=\"1 minute\" \/>\n<script type=\"application\/ld+json\" class=\"yoast-schema-graph\">{\"@context\":\"https:\/\/schema.org\",\"@graph\":[{\"@type\":\"WebPage\",\"@id\":\"https:\/\/svt-dalaine.fr\/svt\/st-d-1-la-rheologie-de-la-lithosphere\/\",\"url\":\"https:\/\/svt-dalaine.fr\/svt\/st-d-1-la-rheologie-de-la-lithosphere\/\",\"name\":\"ST-D-1 La rh\u00e9ologie de la lithosph\u00e8re - Bienvenue sur le site de Sciences de la Vie et de la Terre\",\"isPartOf\":{\"@id\":\"https:\/\/svt-dalaine.fr\/svt\/#website\"},\"datePublished\":\"2024-02-25T09:46:41+00:00\",\"dateModified\":\"2026-02-17T10:31:07+00:00\",\"breadcrumb\":{\"@id\":\"https:\/\/svt-dalaine.fr\/svt\/st-d-1-la-rheologie-de-la-lithosphere\/#breadcrumb\"},\"inLanguage\":\"fr-FR\",\"potentialAction\":[{\"@type\":\"ReadAction\",\"target\":[\"https:\/\/svt-dalaine.fr\/svt\/st-d-1-la-rheologie-de-la-lithosphere\/\"]}]},{\"@type\":\"BreadcrumbList\",\"@id\":\"https:\/\/svt-dalaine.fr\/svt\/st-d-1-la-rheologie-de-la-lithosphere\/#breadcrumb\",\"itemListElement\":[{\"@type\":\"ListItem\",\"position\":1,\"name\":\"Accueil\",\"item\":\"https:\/\/svt-dalaine.fr\/svt\/\"},{\"@type\":\"ListItem\",\"position\":2,\"name\":\"ST-D-1 La rh\u00e9ologie de la lithosph\u00e8re\"}]},{\"@type\":\"WebSite\",\"@id\":\"https:\/\/svt-dalaine.fr\/svt\/#website\",\"url\":\"https:\/\/svt-dalaine.fr\/svt\/\",\"name\":\"Bienvenue sur le site de Sciences de la Vie et de la Terre\",\"description\":\"Ressources en SVT de St\u00e9phanie Dalaine, professeure agr\u00e9g\u00e9e exer\u00e7ant en BCPST1 ENCPB\",\"potentialAction\":[{\"@type\":\"SearchAction\",\"target\":{\"@type\":\"EntryPoint\",\"urlTemplate\":\"https:\/\/svt-dalaine.fr\/svt\/?s={search_term_string}\"},\"query-input\":\"required name=search_term_string\"}],\"inLanguage\":\"fr-FR\"}]}<\/script>\n<!-- \/ Yoast SEO plugin. -->","yoast_head_json":{"title":"ST-D-1 La rh\u00e9ologie de la lithosph\u00e8re - Bienvenue sur le site de Sciences de la Vie et de la Terre","robots":{"index":"index","follow":"follow","max-snippet":"max-snippet:-1","max-image-preview":"max-image-preview:large","max-video-preview":"max-video-preview:-1"},"canonical":"https:\/\/svt-dalaine.fr\/svt\/st-d-1-la-rheologie-de-la-lithosphere\/","og_locale":"fr_FR","og_type":"article","og_title":"ST-D-1 La rh\u00e9ologie de la lithosph\u00e8re - Bienvenue sur le site de Sciences de la Vie et de la Terre","og_description":"Extrait du B.O. Les mat\u00e9riaux lithosph\u00e9riques se d\u00e9forment sous l\u2019effet de contraintes : la d\u00e9formation est r\u00e9versible ou irr\u00e9versible. La d\u00e9formation finie peut se d\u00e9composer en \u00e9tapes (ou incr\u00e9ments) de deux types comportant ou non une part de rotation. Le&hellip;&nbsp;Lire la suite","og_url":"https:\/\/svt-dalaine.fr\/svt\/st-d-1-la-rheologie-de-la-lithosphere\/","og_site_name":"Bienvenue sur le site de Sciences de la Vie et de la Terre","article_modified_time":"2026-02-17T10:31:07+00:00","og_image":[{"url":"https:\/\/svt-dalaine.fr\/svt\/wp-content\/uploads\/2024\/02\/L-tectonique1-768x576.jpg"}],"twitter_card":"summary_large_image","twitter_misc":{"Dur\u00e9e de lecture estim\u00e9e":"1 minute"},"schema":{"@context":"https:\/\/schema.org","@graph":[{"@type":"WebPage","@id":"https:\/\/svt-dalaine.fr\/svt\/st-d-1-la-rheologie-de-la-lithosphere\/","url":"https:\/\/svt-dalaine.fr\/svt\/st-d-1-la-rheologie-de-la-lithosphere\/","name":"ST-D-1 La rh\u00e9ologie de la lithosph\u00e8re - Bienvenue sur le site de Sciences de la Vie et de la Terre","isPartOf":{"@id":"https:\/\/svt-dalaine.fr\/svt\/#website"},"datePublished":"2024-02-25T09:46:41+00:00","dateModified":"2026-02-17T10:31:07+00:00","breadcrumb":{"@id":"https:\/\/svt-dalaine.fr\/svt\/st-d-1-la-rheologie-de-la-lithosphere\/#breadcrumb"},"inLanguage":"fr-FR","potentialAction":[{"@type":"ReadAction","target":["https:\/\/svt-dalaine.fr\/svt\/st-d-1-la-rheologie-de-la-lithosphere\/"]}]},{"@type":"BreadcrumbList","@id":"https:\/\/svt-dalaine.fr\/svt\/st-d-1-la-rheologie-de-la-lithosphere\/#breadcrumb","itemListElement":[{"@type":"ListItem","position":1,"name":"Accueil","item":"https:\/\/svt-dalaine.fr\/svt\/"},{"@type":"ListItem","position":2,"name":"ST-D-1 La rh\u00e9ologie de la lithosph\u00e8re"}]},{"@type":"WebSite","@id":"https:\/\/svt-dalaine.fr\/svt\/#website","url":"https:\/\/svt-dalaine.fr\/svt\/","name":"Bienvenue sur le site de Sciences de la Vie et de la Terre","description":"Ressources en SVT de St\u00e9phanie Dalaine, professeure agr\u00e9g\u00e9e exer\u00e7ant en BCPST1 ENCPB","potentialAction":[{"@type":"SearchAction","target":{"@type":"EntryPoint","urlTemplate":"https:\/\/svt-dalaine.fr\/svt\/?s={search_term_string}"},"query-input":"required name=search_term_string"}],"inLanguage":"fr-FR"}]}},"_links":{"self":[{"href":"https:\/\/svt-dalaine.fr\/svt\/wp-json\/wp\/v2\/pages\/2150","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/svt-dalaine.fr\/svt\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/svt-dalaine.fr\/svt\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/svt-dalaine.fr\/svt\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/svt-dalaine.fr\/svt\/wp-json\/wp\/v2\/comments?post=2150"}],"version-history":[{"count":6,"href":"https:\/\/svt-dalaine.fr\/svt\/wp-json\/wp\/v2\/pages\/2150\/revisions"}],"predecessor-version":[{"id":2161,"href":"https:\/\/svt-dalaine.fr\/svt\/wp-json\/wp\/v2\/pages\/2150\/revisions\/2161"}],"wp:attachment":[{"href":"https:\/\/svt-dalaine.fr\/svt\/wp-json\/wp\/v2\/media?parent=2150"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/svt-dalaine.fr\/svt\/wp-json\/wp\/v2\/categories?post=2150"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/svt-dalaine.fr\/svt\/wp-json\/wp\/v2\/tags?post=2150"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}