{"id":865,"date":"2015-07-21T16:17:17","date_gmt":"2015-07-21T16:17:17","guid":{"rendered":"http:\/\/ground.geophysicsgpr.com\/?page_id=865"},"modified":"2017-03-10T19:21:11","modified_gmt":"2017-03-10T19:21:11","slug":"mineral-exploration","status":"publish","type":"page","link":"https:\/\/ground.geophysicsgpr.com\/en\/techniques\/electrical-resistivity-ip-and-sp\/mineral-exploration","title":{"rendered":"Mineral Exploration"},"content":{"rendered":"<div id=\"pl-865\"  class=\"panel-layout\" ><div id=\"pg-865-0\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-865-0-0\"  class=\"panel-grid-cell\" ><div id=\"panel-865-0-0-0\" 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-865-0-0-0\" ><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><b> For mineral exploration <\/b>, the induced polarization (IP) is often used to find mineralized zones. This is one of the most used ground geophysical methods in mining. The exploration resistivity using a direct current can also be used for non-metallic targets such as some industrial minerals.<\/p>\n<p>For more information, please contact our\u00a0<a href=\"mailto:info@geophysicsgpr.com\">Ground Survey Team<\/a>.<\/p>\n<\/div>\n<\/div><\/div><\/div><\/div><\/div><div id=\"pg-865-1\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-865-1-0\"  class=\"panel-grid-cell\" ><div id=\"panel-865-1-0-0\" 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-865-1-0-0\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-image so-widget-sow-image-default-8b5b6f678277-865\"\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=\"Mineral Exploration\" \t\tclass=\"so-widget-image\"\/>\n\t<\/div>\n\n<\/div><\/div><\/div><\/div><div id=\"pgc-865-1-1\"  class=\"panel-grid-cell\" ><div id=\"panel-865-1-1-0\" 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-865-1-1-0\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-image so-widget-sow-image-default-8b5b6f678277-865\"\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=\"Mineral Exploration\" \t\tclass=\"so-widget-image\"\/>\n\t<\/div>\n\n<\/div><\/div><\/div><\/div><\/div><\/div>","protected":false},"excerpt":{"rendered":"<p>For mineral exploration , the induced polarization (IP) is often used to find mineralized zones. This is one of the most used ground geophysical methods in mining. The exploration resistivity using a direct current can also be used for non-metallic targets such as some industrial minerals.For more information, please contact our\u00a0Ground Survey Team.<\/p>\n","protected":false},"author":1,"featured_media":1118,"parent":844,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"page-full-width.php","meta":{"content-type":"","footnotes":""},"class_list":["post-865","page","type-page","status-publish","has-post-thumbnail","hentry"],"_links":{"self":[{"href":"https:\/\/ground.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/pages\/865","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/ground.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/ground.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/ground.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/ground.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/comments?post=865"}],"version-history":[{"count":2,"href":"https:\/\/ground.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/pages\/865\/revisions"}],"predecessor-version":[{"id":3052,"href":"https:\/\/ground.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/pages\/865\/revisions\/3052"}],"up":[{"embeddable":true,"href":"https:\/\/ground.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/pages\/844"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/ground.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/media\/1118"}],"wp:attachment":[{"href":"https:\/\/ground.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/media?parent=865"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}