{"id":867,"date":"2015-07-21T16:17:17","date_gmt":"2015-07-21T16:17:17","guid":{"rendered":"http:\/\/ground.geophysicsgpr.com\/?page_id=867"},"modified":"2017-02-28T21:36:54","modified_gmt":"2017-02-28T21:36:54","slug":"exploration-miniere","status":"publish","type":"page","link":"https:\/\/ground.geophysicsgpr.com\/fr\/techniques-de-geophysique-terrestre\/resistivite-electrique-pp-ps\/exploration-miniere","title":{"rendered":"Exploration mini\u00e8re"},"content":{"rendered":"<div id=\"pl-867\"  class=\"panel-layout\" ><div id=\"pg-867-0\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-867-0-0\"  class=\"panel-grid-cell\" ><div id=\"panel-867-0-0-0\" 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-867-0-0-0\" ><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>Pour l'exploration mini\u00e8re, la polarisation provoqu\u00e9e (PP) est couramment utilis\u00e9e afin de trouver des zones min\u00e9ralis\u00e9es. C'est une des m\u00e9thodes de g\u00e9ophysique terrestre les plus utilis\u00e9es dans le domaine minier. L'exploration par r\u00e9sistivit\u00e9 \u00e0 l'aide d'un courant continu peut aussi \u00eatre utilis\u00e9e pour des cibles non m\u00e9talliques, telles que certains min\u00e9raux industriels.<\/p>\n<h2 class=\"h2resize\">L'Exploration mini\u00e8re et la conductivit\u00e9 \u00e9lectrique des terrains<\/h2>\n<p>L'exploration mini\u00e8re est l'un des domaines o\u00f9 la g\u00e9ophysique est tr\u00e8s souvent appliqu\u00e9e comme outil de d\u00e9tection directe. Le magn\u00e9tisme est employ\u00e9, syst\u00e9matiquement ou th\u00e9matiquement, dans tous les programmes d'exploration mini\u00e8re.<\/p>\n<p>Les m\u00e9thodes de g\u00e9ophysique terrestre recherchent des anomalies, au niveau de la gravit\u00e9, du magn\u00e9tisme terrestre et de la conductivit\u00e9 \u00e9lectrique des terrains. Les sp\u00e9cialistes sont m\u00eame en mesure d'\u00e9valuer le volume de la masse et sa profondeur. Un gisement riche en fer par exemple pourra donner des anomalies au niveau du magn\u00e9tisme terrestre ou de la conductivit\u00e9 \u00e9lectrique des terrains.<\/p>\n<h3>Dans le domaine de l'exploration mini\u00e8re, la technique de \u00ab polarisation provoqu\u00e9e \u00bb en forage est utilis\u00e9e pour la caract\u00e9risation des gisements afin d'obtenir des renseignements sur la diss\u00e9mination du minerai, ainsi que sa distribution<\/h3>\n<p>L'exemple ci-bas pr\u00e9sente un gisement de phosphate pour lequel un lev\u00e9 g\u00e9ophysique de r\u00e9sistivit\u00e9 \u00e9lectrique \u00e0 haute r\u00e9solution d\u00e9limite clairement la forme du d\u00e9p\u00f4t \u00e9conomique.<\/p>\n<p>\u00a0<\/p>\n<p>\u00a0<\/p>\n<p>Pour plus d'information, veuillez contacter notre <a href=\"mailto:daniel.campos@geophysicsgpr.com;jean-luc.arsenault@geophysicsgpr.com;claude.robillard@geophysicsgpr.com;info@geophysicsgpr.com\">\u00c9quipe de Lev\u00e9 Terrestre<\/a>.<\/p>\n<\/div>\n<\/div><\/div><\/div><\/div><\/div><div id=\"pg-867-1\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-867-1-0\"  class=\"panel-grid-cell\" ><div id=\"panel-867-1-0-0\" 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-867-1-0-0\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-image so-widget-sow-image-default-8b5b6f678277-867\"\n\t\t\t\n\t\t>\n<div class=\"sow-image-container\">\n\t\t<img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/ground.geophysicsgpr.com\/wp-content\/uploads\/sites\/7\/2015\/07\/Ground_Techniques_resistivity_Exploaration.png\" width=\"680\" height=\"142\" srcset=\"https:\/\/ground.geophysicsgpr.com\/wp-content\/uploads\/sites\/7\/2015\/07\/Ground_Techniques_resistivity_Exploaration.png 680w, https:\/\/ground.geophysicsgpr.com\/wp-content\/uploads\/sites\/7\/2015\/07\/Ground_Techniques_resistivity_Exploaration-300x63.png 300w\" sizes=\"auto, (max-width: 680px) 100vw, 680px\" title=\"Ground Techniques resistivity Exploration\" alt=\"Ground Techniques resistivity Exploration\" \t\tclass=\"so-widget-image\"\/>\n\t<\/div>\n\n<\/div><\/div><\/div><\/div><div id=\"pgc-867-1-1\"  class=\"panel-grid-cell\" ><div id=\"panel-867-1-1-0\" 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-867-1-1-0\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-image so-widget-sow-image-default-8b5b6f678277-867\"\n\t\t\t\n\t\t>\n<div class=\"sow-image-container\">\n\t\t<img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/ground.geophysicsgpr.com\/wp-content\/uploads\/sites\/7\/2015\/07\/Ground_Resistivity_Exploration-e1446834373520.jpg\" width=\"213\" height=\"144\" sizes=\"auto, (max-width: 213px) 100vw, 213px\" title=\"Ground Resistivity Exploration\" alt=\"Ground Resistivity Exploration\" \t\tclass=\"so-widget-image\"\/>\n\t<\/div>\n\n<\/div><\/div><\/div><\/div><\/div><\/div>","protected":false},"excerpt":{"rendered":"<p>Pour l&rsquo;exploration mini\u00e8re, la polarisation provoqu\u00e9e (PP) est couramment utilis\u00e9e afin de trouver des zones min\u00e9ralis\u00e9es. C&rsquo;est une des m\u00e9thodes de g\u00e9ophysique terrestre les plus utilis\u00e9es dans le domaine minier. L&rsquo;exploration par r\u00e9sistivit\u00e9 \u00e0 l&rsquo;aide d&rsquo;un courant continu peut aussi \u00eatre utilis\u00e9e pour des cibles non m\u00e9talliques, telles que certains min\u00e9raux industriels.L&rsquo;Exploration mini\u00e8re et la&#8230;  <a href=\"https:\/\/ground.geophysicsgpr.com\/fr\/techniques-de-geophysique-terrestre\/resistivite-electrique-pp-ps\/exploration-miniere\" class=\"more-link\" title=\"Read Exploration mini\u00e8re\">Read more &raquo;<\/a><\/p>\n","protected":false},"author":1,"featured_media":1118,"parent":846,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"page-full-width.php","meta":{"content-type":"","footnotes":""},"class_list":["post-867","page","type-page","status-publish","has-post-thumbnail","hentry"],"_links":{"self":[{"href":"https:\/\/ground.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/pages\/867","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/ground.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/ground.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/ground.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/ground.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/comments?post=867"}],"version-history":[{"count":1,"href":"https:\/\/ground.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/pages\/867\/revisions"}],"predecessor-version":[{"id":3019,"href":"https:\/\/ground.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/pages\/867\/revisions\/3019"}],"up":[{"embeddable":true,"href":"https:\/\/ground.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/pages\/846"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/ground.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/media\/1118"}],"wp:attachment":[{"href":"https:\/\/ground.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/media?parent=867"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}