{"id":6115,"date":"2022-02-03T08:42:35","date_gmt":"2022-02-03T07:42:35","guid":{"rendered":"https:\/\/lyon-geologie.univ-lyon1.fr\/?page_id=6115"},"modified":"2023-01-17T12:12:20","modified_gmt":"2023-01-17T11:12:20","slug":"m1_strati_seq","status":"publish","type":"page","link":"https:\/\/lyongeologie.fr\/en\/m1-geosciences\/m1_strati_seq\/","title":{"rendered":"M1 Stratigraphie s\u00e9quentielle"},"content":{"rendered":"
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Sequence Stratigraphy
<\/strong><\/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
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3 Credits<\/em><\/p>

Contact: Claude COLOMBI\u00c9<\/a>
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\n\t\t\t\t\t\n\t\t\t\t\t\t\n\t\t\t\t\t\t\t\t\tBack 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
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This course has 2 main objectives:<\/p>

    • to determine the spatial and temporal distribution of sediments in sedimentary basins, from dynamic correlations between serial sections and log records based on sequence interpretation;<\/li>
    • to analyze the geometries of sedimentary bodies and the discontinuities that separate them.<\/li><\/ul><\/li><\/ul>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t
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      Sequence stratigraphy is used to understand the spatio-temporal organisation of sedimentary deposits and to determine the factors that control the dynamics of siliciclastic and carbonate systems, and more generally that of our planet.<\/small><\/i><\/figcaption>\n\t\t\t\t\t\t\t\t\t\t<\/figure>\n\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t
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      Elle comprend 4 parties distinctes<\/strong> :<\/p>

          1. presentation of the basic concepts of sequence stratigraphy and the sedimentary processes that underlie them;<\/li>
          2. discussion of the different schools of thought that have evolved these concepts;<\/li>
          3. application of these concepts to the reading, interpretation and correlation of seismic profiles, log records, outcrops, and sedimentological sections;\u00a0<\/li>
          4. estimation of the relative contribution of major factors controlling sedimentary organisation, such as eustatism, subsidence, sedimentary input in terrigenous detrital systems or sedimentary output in carbonate systems.<\/li><\/ol><\/li><\/ol><\/li><\/ol>

            The assessment of this course consists of a continuous and a final assessments, each of which contributes half of the final grade.<\/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

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            \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":"

            Stratigraphie S\u00e9quentielle Cr\u00e9dits : 3 ECTS Responsable : Claude COLOMBI\u00c9 Retour \u00e0 la liste des UEs Dans la foul\u00e9e des UEs P\u00e9trographie s\u00e9dimentaire (L2ST), Faci\u00e8s et processus s\u00e9dimentaire (L3G), Bassins S\u00e9dimentaires (L3G) et Dynamique s\u00e9dimentaire (M1STPE), cette UE a 2 principaux objectifs : d\u00e9terminer la distribution spatiale et temporelle des s\u00e9diments dans les bassins s\u00e9dimentaires, […]<\/p>\n","protected":false},"author":5,"featured_media":0,"parent":511,"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-6115","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/lyongeologie.fr\/en\/wp-json\/wp\/v2\/pages\/6115","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\/5"}],"replies":[{"embeddable":true,"href":"https:\/\/lyongeologie.fr\/en\/wp-json\/wp\/v2\/comments?post=6115"}],"version-history":[{"count":23,"href":"https:\/\/lyongeologie.fr\/en\/wp-json\/wp\/v2\/pages\/6115\/revisions"}],"predecessor-version":[{"id":16333,"href":"https:\/\/lyongeologie.fr\/en\/wp-json\/wp\/v2\/pages\/6115\/revisions\/16333"}],"up":[{"embeddable":true,"href":"https:\/\/lyongeologie.fr\/en\/wp-json\/wp\/v2\/pages\/511"}],"wp:attachment":[{"href":"https:\/\/lyongeologie.fr\/en\/wp-json\/wp\/v2\/media?parent=6115"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}