{"id":100,"date":"2015-07-22T17:40:26","date_gmt":"2015-07-22T16:40:26","guid":{"rendered":"http:\/\/marine.geophysicsgpr.com\/?page_id=100"},"modified":"2017-03-09T17:17:41","modified_gmt":"2017-03-09T16:17:41","slug":"techniques-sismiques-marine","status":"publish","type":"page","link":"https:\/\/marine.geophysicsgpr.com\/fr\/techniques-geophysiques-marine\/techniques-sismiques-marine","title":{"rendered":"Sismique"},"content":{"rendered":"<div id=\"pl-100\"  class=\"panel-layout\" ><div id=\"pg-100-0\"  class=\"panel-grid panel-has-style\" ><div class=\"texte-home-right article panel-row-style panel-row-style-for-100-0\" ><div id=\"pgc-100-0-0\"  class=\"panel-grid-cell\" ><div id=\"panel-100-0-0-0\" class=\"so-panel widget widget_sow-editor panel-first-child panel-last-child\" data-index=\"0\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-editor so-widget-sow-editor-base\"\n\t\t\t\n\t\t>\n<div class=\"siteorigin-widget-tinymce textwidget\">\n\t<h2 class=\"h2resize\">M\u00e9thodes appliqu\u00e9es aux techniques sismiques marine<\/h2>\n<p>Les\u00a0techniques sismiques marine sont semblables aux techniques terrestres mais les m\u00e9thodes doivent inclure des corrections pour la travers\u00e9e du volume d'eau.\u00a0Dans le domaine marin, il existe diff\u00e9rentes m\u00e9thodes d'application de la sismique r\u00e9flexion cherchant \u00e0 identifier des structures \u00e0 plus de 10 ou 20 m\u00e8tres de profondeur sous le fond marin.<\/p>\n<p>La m\u00e9thode de sismique r\u00e9flexion s'appuie sur l'envoi d'une onde sismique dans le fond marin et sur l'enregistrement des ondes refl\u00e9t\u00e9es par les couches g\u00e9ologiques sous-jacentes.<\/p>\n<p>Les techniques de sismique marine sont bas\u00e9es sur les principes de la <a href=\"http:\/\/marine.geophysicsgpr.com\/fr\/techniques-geophysiques-marine\/techniques-sismiques-marine\/reflexion\">sismique r\u00e9flexion<\/a>; envoi d'une onde sismique dans le fond marin et \u00e9coute des ondes refl\u00e9t\u00e9es par des couches g\u00e9ologiques.<\/p>\n<p>\u00a0<\/p>\n<p>\u00a0<\/p>\n<p>Pour plus d'informations, veuillez contacter notre <span style=\"color: #013ca6\"><a style=\"color: #013ca6\" href=\"mailto:info@geophysicsgpr.com\">\u00c9quipe de lev\u00e9 marin<\/a><\/span>.<\/p>\n<p>\u00a0<\/p>\n<\/div>\n<\/div><\/div><\/div><\/div><\/div><div id=\"pg-100-1\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-100-1-0\"  class=\"panel-grid-cell\" ><div id=\"panel-100-1-0-0\" class=\"so-panel widget widget_black-studio-tinymce widget_black_studio_tinymce panel-first-child panel-last-child\" data-index=\"1\" ><div class=\"textwidget\"><p><div id=\"wondergridgallerylightbox_options\" data-skinsfoldername=\"skins\/default\/\"  data-jsfolder=\"https:\/\/marine.geophysicsgpr.com\/wp-content\/plugins\/wonderplugin-gridgallery\/engine\/\" style=\"display:none;\"><\/div>\r\n<style type=\"text\/css\">.wpp-btn-blue-medium {     background: #fa4c06; 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font-size:14px; font-family:Armata,sans-serif,Arial; overflow:hidden; text-align:left;}\" data-descriptionbottomcss=\"{color:#333; font-size:12px; font-family:Arial,Helvetica,sans-serif; overflow:hidden; text-align:left; margin:4px 0px 0px; padding: 0px;}\" data-googleanalyticsaccount=\"\" data-gap=\"4\" data-margin=\"10\" data-borderradius=\"0\" data-hoverzoominvalue=\"24\" data-hoverzoominduration=\"180\" data-hoverzoominimagescale=\"1.1\" data-hoverzoominimageduration=\"360\" data-hoverfadeopacity=\"0.8\" data-hoverfadeduration=\"300\" data-videoplaybutton=\"playvideo-64-64-0.png\" data-column=\"3\" data-mediumcolumn=\"2\" data-mediumscreensize=\"800\" data-smallcolumn=\"1\" data-smallscreensize=\"600\" data-titlemode=\"always\" data-titleeffect=\"fade\" data-titleeffectduration=\"500\" data-titleheight=\"0\" data-jsfolder=\"https:\/\/marine.geophysicsgpr.com\/wp-content\/plugins\/wonderplugin-gridgallery\/engine\/\" data-skinsfoldername=\"skins\/default\/\" style=\"display:none;position:relative;margin:0 auto;width:100%;max-width:1328px;\" ><div class=\"wonderplugin-gridgallery-list\" style=\"display:block;position:relative;max-width:100%;margin:0 auto;\"><div class=\"wonderplugin-gridgallery-item\" data-row=\"1\" data-col=\"1\"><div class=\"wonderplugin-gridgallery-item-container\"><a href=\"http:\/\/marine.geophysicsgpr.com\/fr\/techniques-geophysiques-marine\/techniques-sismiques-marine\/refraction\" title=\"R\u00e9fraction\" data-description=\"G\u00e9ophysique GPR se sp\u00e9cialise en \u00e9tudes de sismique r\u00e9fraction dans le cadre de recherches en g\u00e9nie, en g\u00e9otechnique et en g\u00e9ologie.\" data-button=\"<a href=&quot;http:\/\/marine.geophysicsgpr.com\/fr\/techniques-geophysiques-marine\/techniques-sismiques-marine\/refraction&quot;><button class=&quot;wpp-btn-blue-medium&quot;>En savoir plus<\/button><\/a>\"><img decoding=\"async\" class=\"wonderplugin-gridgallery-item-img\" src=\"http:\/\/marine.geophysicsgpr.com\/wp-content\/uploads\/sites\/5\/2015\/07\/Marine_techniques_seismic_inset.jpg\" \/><\/a><\/div><\/div><div class=\"wonderplugin-gridgallery-item\" data-row=\"1\" data-col=\"1\"><div class=\"wonderplugin-gridgallery-item-container\"><a href=\"http:\/\/marine.geophysicsgpr.com\/fr\/techniques\/sismique\/reflexion\" title=\"R\u00e9flexion\" data-description=\"La m\u00e9thode de sismique r\u00e9flexion s\u2019appuie sur l\u2019envoi d\u2019une onde sismique dans le fond marin et sur l\u2019enregistrement des ondes refl\u00e9t\u00e9es par les couches g\u00e9ologiques sous-jacentes.\" data-button=\"<a href=&quot;http:\/\/marine.geophysicsgpr.com\/fr\/techniques\/sismique\/reflexion&quot;><button class=&quot;wpp-btn-blue-medium&quot;>En savoir plus<\/button><\/a>\"><img decoding=\"async\" class=\"wonderplugin-gridgallery-item-img\" src=\"http:\/\/marine.geophysicsgpr.com\/wp-content\/uploads\/sites\/5\/2015\/08\/Marine_Technic_Seismic.png\" \/><\/a><\/div><\/div><div class=\"wonderplugin-gridgallery-item\" data-row=\"1\" data-col=\"1\"><div class=\"wonderplugin-gridgallery-item-container\"><a href=\"http:\/\/marine.geophysicsgpr.com\/fr\/techniques\/sismique\/amos-masw\" title=\"AMOS (MASW)\" data-description=\"L\u2019analyse multicanale des ondes de surface (MASW) est une m\u00e9thode sismique qui permet de calculer la vitesse d\u2019onde.\" data-button=\"<a href=&quot;http:\/\/marine.geophysicsgpr.com\/fr\/techniques\/sismique\/amos-masw&quot;><button class=&quot;wpp-btn-blue-medium&quot;>En savoir plus<\/button><\/a>\"><img decoding=\"async\" class=\"wonderplugin-gridgallery-item-img\" src=\"http:\/\/marine.geophysicsgpr.com\/wp-content\/uploads\/sites\/5\/2015\/08\/Marine_Technic_Seismic_MASW.jpg\" \/><\/a><\/div><\/div><div style=\"clear:both;\"><\/div><\/div><div class=\"wonderplugin-gridgallery-engine\"><a href=\"http:\/\/www.wonderplugin.com\/wordpress-gridgallery\/\" title=\"WordPress Grid Gallery\">WordPress Grid Gallery<\/a><\/div><\/div><\/p>\n<\/div><\/div><\/div><\/div><\/div>","protected":false},"excerpt":{"rendered":"<p>M\u00e9thodes appliqu\u00e9es aux techniques sismiques marineLes\u00a0techniques sismiques marine sont semblables aux techniques terrestres mais les m\u00e9thodes doivent inclure des corrections pour la travers\u00e9e du volume d&rsquo;eau.\u00a0Dans le domaine marin, il existe diff\u00e9rentes m\u00e9thodes d&rsquo;application de la sismique r\u00e9flexion cherchant \u00e0 identifier des structures \u00e0 plus de 10 ou 20 m\u00e8tres de profondeur sous le fond&#8230;  <a href=\"https:\/\/marine.geophysicsgpr.com\/fr\/techniques-geophysiques-marine\/techniques-sismiques-marine\" class=\"more-link\" title=\"Read Sismique\">Read more &raquo;<\/a><\/p>\n","protected":false},"author":1,"featured_media":78,"parent":16,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"page-full-width.php","meta":{"content-type":"","footnotes":""},"class_list":["post-100","page","type-page","status-publish","has-post-thumbnail","hentry"],"_links":{"self":[{"href":"https:\/\/marine.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/pages\/100","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/marine.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/marine.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/marine.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/marine.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/comments?post=100"}],"version-history":[{"count":13,"href":"https:\/\/marine.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/pages\/100\/revisions"}],"predecessor-version":[{"id":1612,"href":"https:\/\/marine.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/pages\/100\/revisions\/1612"}],"up":[{"embeddable":true,"href":"https:\/\/marine.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/pages\/16"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/marine.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/media\/78"}],"wp:attachment":[{"href":"https:\/\/marine.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/media?parent=100"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}