{"id":8,"date":"2025-09-30T13:15:37","date_gmt":"2025-09-30T11:15:37","guid":{"rendered":"https:\/\/geops.geol.u-psud.fr\/br\/?page_id=8"},"modified":"2026-03-05T12:03:27","modified_gmt":"2026-03-05T11:03:27","slug":"accueil-bassins-ressources","status":"publish","type":"page","link":"https:\/\/geops.geol.u-psud.fr\/br\/","title":{"rendered":"Accueil Bassins &#038; Ressources"},"content":{"rendered":"<p><div class=\"fusion-fullwidth fullwidth-box fusion-builder-row-1 fusion-flex-container has-pattern-background has-mask-background nonhundred-percent-fullwidth non-hundred-percent-height-scrolling\" style=\"--awb-border-radius-top-left:0px;--awb-border-radius-top-right:0px;--awb-border-radius-bottom-right:0px;--awb-border-radius-bottom-left:0px;--awb-flex-wrap:wrap;\" ><div class=\"fusion-builder-row fusion-row fusion-flex-align-items-flex-start fusion-flex-content-wrap\" style=\"max-width:1248px;margin-left: calc(-4% \/ 2 );margin-right: calc(-4% \/ 2 );\"><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-0 fusion_builder_column_1_1 1_1 fusion-flex-column\" style=\"--awb-bg-size:cover;--awb-width-large:100%;--awb-margin-top-large:0px;--awb-spacing-right-large:1.92%;--awb-margin-bottom-large:20px;--awb-spacing-left-large:1.92%;--awb-width-medium:100%;--awb-order-medium:0;--awb-spacing-right-medium:1.92%;--awb-spacing-left-medium:1.92%;--awb-width-small:100%;--awb-order-small:0;--awb-spacing-right-small:1.92%;--awb-spacing-left-small:1.92%;\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\"><div class=\"fusion-title title fusion-title-1 fusion-sep-none fusion-title-text fusion-title-size-one\" style=\"--awb-margin-top-small:10px;--awb-margin-right-small:0px;--awb-margin-bottom-small:10px;--awb-margin-left-small:0px;\"><h1 class=\"fusion-title-heading title-heading-left fusion-responsive-typography-calculated\" style=\"margin:0;--fontSize:62;line-height:var(--awb-typography1-line-height);\">Bassins &amp; Ressources (B&amp;R)<\/h1><\/div><div class=\"fusion-text fusion-text-1\"><p>Le th\u00e8me \u00ab Bassins &amp; Ressources \u00bb (B&amp;R) s\u2019int\u00e9resse \u00e0 l\u2019\u00e9volution et \u00e0 la dynamique de la lithosph\u00e8re, notamment \u00e0 travers l\u2019\u00e9tude des bassins s\u00e9dimentaires, par des approches s\u00e9dimentologiques, diag\u00e9n\u00e9tiques, structurales, g\u00e9ochimiques, g\u00e9ochronologiques et g\u00e9ophysiques. Les grandes \u00e9tapes et les m\u00e9canismes \u00e0 l\u2019origine de l\u2019\u00e9volution de ces bassins, notamment en domaine intraplaque, sont reconstitu\u00e9es. Les grandes th\u00e9matiques abord\u00e9es concernent (i) les liens entre environnements de d\u00e9p\u00f4t et \u00e9volution diag\u00e9n\u00e9tique des r\u00e9servoirs s\u00e9dimentaires, (ii) les transferts de mati\u00e8re depuis les zones \u00e0 l\u2019\u00e9rosion vers les zones de d\u00e9p\u00f4t (approche <em>source to sink<\/em>), (iii) les moteurs et modalit\u00e9s des circulations des fluides \u00e0 l\u2019origine d\u2019accumulation de ressources (m\u00e9taux, g\u00e9othermie, gaz\u00a0: h\u00e9lium et hydrog\u00e8ne naturel) et (iv) le contr\u00f4le g\u00e9odynamique sur ces diff\u00e9rents ph\u00e9nom\u00e8nes.<\/p>\n<p>Les animateurs du th\u00e8me sont <a href=\"https:\/\/geops.geol.u-psud.fr\/user\/bbrigau\/\">Benjamin Brigaud<\/a> et <a href=\"https:\/\/geops.geol.u-psud.fr\/user\/tblaise1\/\">Thomas Blaise<\/a>.<\/p>\n<\/div><\/div><\/div><\/div><\/div><div class=\"fusion-fullwidth fullwidth-box fusion-builder-row-2 fusion-flex-container has-pattern-background has-mask-background nonhundred-percent-fullwidth non-hundred-percent-height-scrolling\" style=\"--awb-border-sizes-top:30px;--awb-border-sizes-bottom:30px;--awb-border-sizes-left:30px;--awb-border-sizes-right:30px;--awb-border-radius-top-left:0px;--awb-border-radius-top-right:0px;--awb-border-radius-bottom-right:0px;--awb-border-radius-bottom-left:0px;--awb-background-color:var(--awb-color3);--awb-flex-wrap:wrap;\" ><div class=\"fusion-builder-row fusion-row fusion-flex-align-items-flex-start fusion-flex-content-wrap\" style=\"max-width:1248px;margin-left: calc(-4% \/ 2 );margin-right: calc(-4% \/ 2 );\"><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-1 fusion_builder_column_1_1 1_1 fusion-flex-column\" style=\"--awb-bg-size:cover;--awb-width-large:100%;--awb-margin-top-large:0px;--awb-spacing-right-large:1.92%;--awb-margin-bottom-large:20px;--awb-spacing-left-large:1.92%;--awb-width-medium:100%;--awb-order-medium:0;--awb-spacing-right-medium:1.92%;--awb-spacing-left-medium:1.92%;--awb-width-small:100%;--awb-order-small:0;--awb-spacing-right-small:1.92%;--awb-spacing-left-small:1.92%;\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\"><div class=\"fusion-title title fusion-title-2 fusion-sep-none fusion-title-text fusion-title-size-two\" style=\"--awb-margin-top-small:10px;--awb-margin-right-small:0px;--awb-margin-bottom-small:10px;--awb-margin-left-small:0px;\"><h2 class=\"fusion-title-heading title-heading-left fusion-responsive-typography-calculated\" style=\"margin:0;--fontSize:46;line-height:var(--awb-typography1-line-height);\">Les th\u00e9matiques<\/h2><\/div><\/div><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-2 fusion_builder_column_1_3 1_3 fusion-flex-column fusion-column-inner-bg-wrapper\" style=\"--awb-padding-top:40px;--awb-padding-right:30px;--awb-padding-bottom:40px;--awb-padding-left:30px;--awb-inner-bg-color:var(--awb-color1);--awb-inner-bg-color-hover:var(--awb-color1);--awb-inner-bg-size:cover;--awb-width-large:33.333333333333%;--awb-margin-top-large:30px;--awb-spacing-right-large:5.76%;--awb-margin-bottom-large:30px;--awb-spacing-left-large:5.76%;--awb-width-medium:33.333333333333%;--awb-order-medium:0;--awb-spacing-right-medium:5.76%;--awb-spacing-left-medium:5.76%;--awb-width-small:100%;--awb-order-small:0;--awb-spacing-right-small:1.92%;--awb-spacing-left-small:1.92%;\" data-scroll-devices=\"small-visibility,medium-visibility,large-visibility\"><span class=\"fusion-column-inner-bg hover-type-none\"><a class=\"fusion-column-anchor\" href=\"https:\/\/geops.geol.u-psud.fr\/br\/evolution-sedimentaire-et-diagenetique-des-reservoirs-application-au-stockage\/\"><span class=\"fusion-column-inner-bg-image\"><\/span><\/a><\/span><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\"><i class=\"fb-icon-element-1 fb-icon-element fontawesome-icon fa-flask fas circle-yes\" style=\"--awb-circlecolor:var(--awb-color8);--awb-circlecolor-hover:var(--awb-color8);--awb-circlebordercolor-hover:var(--awb-color8);--awb-circlebordersize:1px;--awb-font-size:22px;--awb-width:44px;--awb-height:44px;--awb-line-height:42px;--awb-margin-top:0;--awb-margin-right:0;--awb-margin-bottom:0;--awb-margin-left:0;--awb-align-self:center;\"><\/i><div class=\"fusion-text fusion-text-2\" style=\"--awb-font-size:28px;--awb-line-height:1.2;--awb-text-color:var(--awb-custom_color_1);--awb-text-font-family:&quot;Figtree&quot;;--awb-text-font-style:normal;--awb-text-font-weight:400;\"><p style=\"text-align: center;\"><strong>E<\/strong><strong>volution s\u00e9dimentaire et <\/strong><strong>diag\u00e9n\u00e9tique<\/strong><strong> des r<\/strong><strong>\u00e9servoirs<\/strong><\/p>\n<\/div><div class=\"fusion-text fusion-text-3\" style=\"--awb-text-color:var(--awb-color8);\"><p style=\"text-align: center;\"><strong>Projets associ\u00e9s :<\/strong><\/p>\n<\/div><div class=\"fusion-text fusion-text-4\" style=\"--awb-text-color:var(--awb-color8);\"><p style=\"text-align: center;\">Contro\u0302les des he\u0301te\u0301roge\u0301ne\u0301ite\u0301s ge\u0301ologiques multi-e\u0301chelle sur les proprie\u0301te\u0301s physiques des roches du Ce\u0301nozoi\u0308que du bassin de Paris : de l\u2019e\u0301chantillon au bassin se\u0301dimentaire<\/p>\n<p style=\"text-align: center;\">Capacite\u0301 re\u0301servoir des formations jurassiques du nord du bassin aquitain<\/p>\n<\/div><\/div><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-3 fusion_builder_column_1_3 1_3 fusion-flex-column fusion-column-inner-bg-wrapper\" style=\"--awb-padding-top:40px;--awb-padding-right:30px;--awb-padding-bottom:40px;--awb-padding-left:30px;--awb-inner-bg-color:var(--awb-color1);--awb-inner-bg-color-hover:var(--awb-color1);--awb-inner-bg-size:cover;--awb-width-large:33.333333333333%;--awb-margin-top-large:30px;--awb-spacing-right-large:5.76%;--awb-margin-bottom-large:30px;--awb-spacing-left-large:5.76%;--awb-width-medium:33.333333333333%;--awb-order-medium:0;--awb-spacing-right-medium:5.76%;--awb-spacing-left-medium:5.76%;--awb-width-small:100%;--awb-order-small:0;--awb-spacing-right-small:1.92%;--awb-spacing-left-small:1.92%;\" data-scroll-devices=\"small-visibility,medium-visibility,large-visibility\"><span class=\"fusion-column-inner-bg hover-type-none\"><a class=\"fusion-column-anchor\" href=\"https:\/\/geops.geol.u-psud.fr\/br\/de-lerosion-aux-zones-de-depot-approche-integree-des-flux-sedimentaires\/\"><span class=\"fusion-column-inner-bg-image\"><\/span><\/a><\/span><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\"><i class=\"fb-icon-element-2 fb-icon-element fontawesome-icon fa-wind fas circle-yes\" style=\"--awb-circlecolor:var(--awb-color8);--awb-circlecolor-hover:var(--awb-color8);--awb-circlebordercolor-hover:var(--awb-color8);--awb-circlebordersize:1px;--awb-font-size:22px;--awb-width:44px;--awb-height:44px;--awb-line-height:42px;--awb-margin-top:0;--awb-margin-right:0;--awb-margin-bottom:0;--awb-margin-left:0;--awb-align-self:center;\"><\/i><div class=\"fusion-text fusion-text-5\" style=\"--awb-font-size:28px;--awb-line-height:1.2;--awb-text-color:var(--awb-custom_color_1);--awb-text-font-family:&quot;Figtree&quot;;--awb-text-font-style:normal;--awb-text-font-weight:400;\"><p style=\"text-align: center;\"><strong>D<\/strong><strong>e l\u2019\u00e9rosion aux zones de d\u00e9p\u00f4t\u00a0: approche int\u00e9gr\u00e9<\/strong><strong>e<\/strong><strong> des flux s\u00e9dimentaires<\/strong><\/p>\n<\/div><div class=\"fusion-text fusion-text-6\" style=\"--awb-text-color:var(--awb-color8);\"><p style=\"text-align: center;\"><strong>Projets associ\u00e9s :<\/strong><\/p>\n<\/div><div class=\"fusion-text fusion-text-7\"><p style=\"text-align: center;\">Variabilite\u0301 spatiale et caracte\u0301risation des facie\u0300s carbonate\u0301s, argileux et e\u0301vaporitiques du Ce\u0301nozoi\u0308que, a\u0300 haute re\u0301solution dans l\u2019emprise du Grand Paris<\/p>\n<\/div><\/div><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-4 fusion_builder_column_1_3 1_3 fusion-flex-column fusion-column-inner-bg-wrapper\" style=\"--awb-padding-top:40px;--awb-padding-right:30px;--awb-padding-bottom:40px;--awb-padding-left:30px;--awb-inner-bg-color:var(--awb-color1);--awb-inner-bg-color-hover:var(--awb-color1);--awb-inner-bg-size:cover;--awb-width-large:33.333333333333%;--awb-margin-top-large:30px;--awb-spacing-right-large:5.76%;--awb-margin-bottom-large:30px;--awb-spacing-left-large:5.76%;--awb-width-medium:33.333333333333%;--awb-order-medium:0;--awb-spacing-right-medium:5.76%;--awb-spacing-left-medium:5.76%;--awb-width-small:100%;--awb-order-small:0;--awb-spacing-right-small:1.92%;--awb-spacing-left-small:1.92%;\" data-scroll-devices=\"small-visibility,medium-visibility,large-visibility\"><span class=\"fusion-column-inner-bg hover-type-none\"><a class=\"fusion-column-anchor\" href=\"https:\/\/geops.geol.u-psud.fr\/br\/geologie-de-la-ressource-pour-la-transition-energetique-applications-aux-metaux-f-li-et-a-la-geothermie\/\"><span class=\"fusion-column-inner-bg-image\"><\/span><\/a><\/span><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\"><i class=\"fb-icon-element-3 fb-icon-element fontawesome-icon fa-redo-alt fas circle-yes\" style=\"--awb-circlecolor:var(--awb-color8);--awb-circlecolor-hover:var(--awb-color8);--awb-circlebordercolor-hover:var(--awb-color8);--awb-circlebordersize:1px;--awb-font-size:22px;--awb-width:44px;--awb-height:44px;--awb-line-height:42px;--awb-margin-top:0;--awb-margin-right:0;--awb-margin-bottom:0;--awb-margin-left:0;--awb-align-self:center;\"><\/i><div class=\"fusion-text fusion-text-8\" style=\"--awb-font-size:28px;--awb-line-height:1.2;--awb-text-color:var(--awb-custom_color_1);--awb-text-font-family:&quot;Figtree&quot;;--awb-text-font-style:normal;--awb-text-font-weight:400;\"><p style=\"text-align: center;\"><strong>G\u00e9ologie de la ressource pour la transition \u00e9nerg\u00e9tique : applications aux m\u00e9taux (Li,\u2026), gaz (He et H<sub>2<\/sub>) et \u00e0 la g\u00e9othermie<\/strong><\/p>\n<\/div><div class=\"fusion-text fusion-text-9\" style=\"--awb-text-color:var(--awb-color8);\"><p style=\"text-align: center;\"><strong>Projets associ\u00e9s :<\/strong><\/p>\n<\/div><div class=\"fusion-text fusion-text-10\"><p style=\"text-align: center;\">H2IDF<br \/>\nPIROS<br \/>\nS-PASS<br \/>\nTHERMOPARIS<br \/>\nIntegrated reservoir characterization of the Grande Oolithe (Dogger) in the Rhine Graben (petrophysics, sedimentology and structural geology)<br \/>\nPR3DICT<br \/>\nCaract\u00e9risation multi-\u00e9chelle de la porosit\u00e9 du r\u00e9servoir de la craie par une approche couplant g\u00e9ologie, p\u00e9trophysique et g\u00e9ophysique<br \/>\nURALOD<br \/>\nROCS<br \/>\nHyperSP<\/p>\n<\/div><\/div><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-5 fusion_builder_column_1_3 1_3 fusion-flex-column fusion-column-inner-bg-wrapper\" style=\"--awb-padding-top:40px;--awb-padding-right:30px;--awb-padding-bottom:40px;--awb-padding-left:30px;--awb-inner-bg-color:var(--awb-color1);--awb-inner-bg-color-hover:var(--awb-color1);--awb-inner-bg-size:cover;--awb-width-large:33.333333333333%;--awb-margin-top-large:30px;--awb-spacing-right-large:5.76%;--awb-margin-bottom-large:30px;--awb-spacing-left-large:5.76%;--awb-width-medium:33.333333333333%;--awb-order-medium:0;--awb-spacing-right-medium:5.76%;--awb-spacing-left-medium:5.76%;--awb-width-small:100%;--awb-order-small:0;--awb-spacing-right-small:1.92%;--awb-spacing-left-small:1.92%;\" data-scroll-devices=\"small-visibility,medium-visibility,large-visibility\"><span class=\"fusion-column-inner-bg hover-type-none\"><a class=\"fusion-column-anchor\" href=\"https:\/\/geops.geol.u-psud.fr\/br\/controle-geodynamique-sur-levolution-des-domaines-intraplaques\/\"><span class=\"fusion-column-inner-bg-image\"><\/span><\/a><\/span><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\"><i class=\"fb-icon-element-4 fb-icon-element fontawesome-icon fa-redo-alt fas circle-yes\" style=\"--awb-circlecolor:var(--awb-color8);--awb-circlecolor-hover:var(--awb-color8);--awb-circlebordercolor-hover:var(--awb-color8);--awb-circlebordersize:1px;--awb-font-size:22px;--awb-width:44px;--awb-height:44px;--awb-line-height:42px;--awb-margin-top:0;--awb-margin-right:0;--awb-margin-bottom:0;--awb-margin-left:0;--awb-align-self:center;\"><\/i><div class=\"fusion-text fusion-text-11\" style=\"--awb-font-size:28px;--awb-line-height:1.2;--awb-text-color:var(--awb-custom_color_1);--awb-text-font-family:&quot;Figtree&quot;;--awb-text-font-style:normal;--awb-text-font-weight:400;\"><p style=\"text-align: center;\"><strong>Contr\u00f4le g\u00e9odynamique sur l\u2019\u00e9volution des domaines intraplaques<\/strong><\/p>\n<\/div><div class=\"fusion-text fusion-text-12\" style=\"--awb-text-color:var(--awb-color8);\"><p style=\"text-align: center;\"><strong>Projets associ\u00e9s :<\/strong><\/p>\n<\/div><\/div><\/div><\/div><\/div><div class=\"fusion-fullwidth fullwidth-box fusion-builder-row-3 fusion-flex-container has-pattern-background has-mask-background nonhundred-percent-fullwidth non-hundred-percent-height-scrolling\" style=\"--awb-border-radius-top-left:0px;--awb-border-radius-top-right:0px;--awb-border-radius-bottom-right:0px;--awb-border-radius-bottom-left:0px;--awb-flex-wrap:wrap;\" ><div class=\"fusion-builder-row fusion-row fusion-flex-align-items-flex-start fusion-flex-content-wrap\" style=\"max-width:1248px;margin-left: calc(-4% \/ 2 );margin-right: calc(-4% \/ 2 );\"><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-6 fusion_builder_column_1_1 1_1 fusion-flex-column\" style=\"--awb-bg-size:cover;--awb-width-large:100%;--awb-margin-top-large:0px;--awb-spacing-right-large:1.92%;--awb-margin-bottom-large:20px;--awb-spacing-left-large:1.92%;--awb-width-medium:100%;--awb-order-medium:0;--awb-spacing-right-medium:1.92%;--awb-spacing-left-medium:1.92%;--awb-width-small:100%;--awb-order-small:0;--awb-spacing-right-small:1.92%;--awb-spacing-left-small:1.92%;\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\"><\/div><\/div><\/div><\/div><\/p>\n","protected":false},"excerpt":{"rendered":"","protected":false},"author":1,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-8","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/geops.geol.u-psud.fr\/br\/wp-json\/wp\/v2\/pages\/8","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/geops.geol.u-psud.fr\/br\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/geops.geol.u-psud.fr\/br\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/geops.geol.u-psud.fr\/br\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/geops.geol.u-psud.fr\/br\/wp-json\/wp\/v2\/comments?post=8"}],"version-history":[{"count":28,"href":"https:\/\/geops.geol.u-psud.fr\/br\/wp-json\/wp\/v2\/pages\/8\/revisions"}],"predecessor-version":[{"id":246,"href":"https:\/\/geops.geol.u-psud.fr\/br\/wp-json\/wp\/v2\/pages\/8\/revisions\/246"}],"wp:attachment":[{"href":"https:\/\/geops.geol.u-psud.fr\/br\/wp-json\/wp\/v2\/media?parent=8"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}