{"id":156,"date":"2015-07-22T17:55:54","date_gmt":"2015-07-22T16:55:54","guid":{"rendered":"http:\/\/marine.geophysicsgpr.com\/?page_id=156"},"modified":"2017-03-09T17:28:42","modified_gmt":"2017-03-09T16:28:42","slug":"mines-et-exploration-miniere","status":"publish","type":"page","link":"https:\/\/marine.geophysicsgpr.com\/fr\/applications-geophysique-marine\/mines-et-exploration-miniere","title":{"rendered":"Mines et exploration mini\u00e8re"},"content":{"rendered":"<div id=\"pl-156\"  class=\"panel-layout\" ><div id=\"pg-156-0\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-156-0-0\"  class=\"panel-grid-cell\" ><div id=\"panel-156-0-0-0\" class=\"so-panel widget widget_sow-editor panel-first-child panel-last-child\" data-index=\"0\" ><div class=\"texte-home-right article panel-widget-style panel-widget-style-for-156-0-0-0\" ><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<p>Les variations locales du champ magn\u00e9tique sont souvent caus\u00e9es par les objets contenant du fer ou d'autres m\u00e9taux magn\u00e9tiques. Il est alors possible de rep\u00e9rer des objets se trouvant submerg\u00e9s, et en rattachant les valeurs par le positionnement GPS, de cr\u00e9er des cartes des variations du champ magn\u00e9tique. G\u00e9ophysique GPR offre une vaste gamme de services g\u00e9ophysiques marins qui pourraient s\u2019appliquer \u00e0 une mine d\u00e9j\u00e0 existante ou \u00e0 un site d\u2019exploration mini\u00e8re.<\/p>\n<h2 class=\"h2resize\">Les lev\u00e9s de magn\u00e9tom\u00e9trie marine<\/h2>\n<p>La cartographie des anomalies magn\u00e9tiques permet la d\u00e9tection des obstructions m\u00e9talliques. La cartographie magn\u00e9tique a d\u00e9montr\u00e9 r\u00e9cemment l'apport de ce type de mesures pour la d\u00e9tection de mines enfouies.<\/p>\n<h2 class=\"h2resize\">Application de la g\u00e9ophysique marine pour les mines et site d'exploration mini\u00e8re.<\/h2>\n<ul>\n<li>Cartographie de la profondeur du substratum rocheux;<\/li>\n<li>Profil g\u00e9ologique et cartographie du sous-sol du fond marin;<\/li>\n<li>Magn\u00e9tom\u00e8tre marin;<\/li>\n<li>\u00c9tude environnementale sur un lit de lac ou un bassin de r\u00e9sidus miniers;<\/li>\n<li>Services de s\u00e9curit\u00e9 marine;<\/li>\n<li>\u00c9tude d\u2019am\u00e9nagement de port.<\/li>\n<\/ul>\n<p>\u00a0<\/p>\n<p>\u00a0<\/p>\n<p>Pour plus d'information, 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<\/div>\n<\/div><\/div><\/div><\/div><\/div><div id=\"pg-156-1\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-156-1-0\"  class=\"panel-grid-cell\" ><div id=\"panel-156-1-0-0\" class=\"so-panel widget widget_sow-image panel-first-child panel-last-child\" data-index=\"1\" ><div class=\"panel-widget-style panel-widget-style-for-156-1-0-0\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-image so-widget-sow-image-default-8b5b6f678277-156\"\n\t\t\t\n\t\t>\n<div class=\"sow-image-container\">\n\t\t<img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/marine.geophysicsgpr.com\/wp-content\/uploads\/sites\/5\/2015\/07\/Marine_applications_mining.jpg\" width=\"640\" height=\"480\" srcset=\"https:\/\/marine.geophysicsgpr.com\/wp-content\/uploads\/sites\/5\/2015\/07\/Marine_applications_mining.jpg 640w, https:\/\/marine.geophysicsgpr.com\/wp-content\/uploads\/sites\/5\/2015\/07\/Marine_applications_mining-300x225.jpg 300w\" sizes=\"auto, (max-width: 640px) 100vw, 640px\" title=\"Mines et exploration mini\u00e8re\" alt=\"exploration mini\u00e8re\" \t\tclass=\"so-widget-image\"\/>\n\t<\/div>\n\n<\/div><\/div><\/div><\/div><div id=\"pgc-156-1-1\"  class=\"panel-grid-cell\" ><div id=\"panel-156-1-1-0\" class=\"so-panel widget widget_sow-image panel-first-child panel-last-child\" data-index=\"2\" ><div class=\"panel-widget-style panel-widget-style-for-156-1-1-0\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-image so-widget-sow-image-default-8b5b6f678277-156\"\n\t\t\t\n\t\t>\n<div class=\"sow-image-container\">\n\t\t<img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/marine.geophysicsgpr.com\/wp-content\/uploads\/sites\/5\/2015\/07\/Marine_applications_min_ex_inset.jpg\" width=\"225\" height=\"228\" sizes=\"auto, (max-width: 225px) 100vw, 225px\" title=\"Marine_applications_min_ex_inset\" alt=\"exploration mini\u00e8re\" \t\tclass=\"so-widget-image\"\/>\n\t<\/div>\n\n<\/div><\/div><\/div><\/div><\/div><\/div>","protected":false},"excerpt":{"rendered":"<p>Les variations locales du champ magn\u00e9tique sont souvent caus\u00e9es par les objets contenant du fer ou d&rsquo;autres m\u00e9taux magn\u00e9tiques. Il est alors possible de rep\u00e9rer des objets se trouvant submerg\u00e9s, et en rattachant les valeurs par le positionnement GPS, de cr\u00e9er des cartes des variations du champ magn\u00e9tique. G\u00e9ophysique GPR offre une vaste gamme de&#8230;  <a href=\"https:\/\/marine.geophysicsgpr.com\/fr\/applications-geophysique-marine\/mines-et-exploration-miniere\" class=\"more-link\" title=\"Read Mines et exploration mini\u00e8re\">Read more &raquo;<\/a><\/p>\n","protected":false},"author":1,"featured_media":78,"parent":21,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"page-full-width.php","meta":{"content-type":"","footnotes":""},"class_list":["post-156","page","type-page","status-publish","has-post-thumbnail","hentry"],"_links":{"self":[{"href":"https:\/\/marine.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/pages\/156","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=156"}],"version-history":[{"count":13,"href":"https:\/\/marine.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/pages\/156\/revisions"}],"predecessor-version":[{"id":1621,"href":"https:\/\/marine.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/pages\/156\/revisions\/1621"}],"up":[{"embeddable":true,"href":"https:\/\/marine.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/pages\/21"}],"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=156"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}