{"id":1171,"date":"2026-01-22T20:04:08","date_gmt":"2026-01-22T23:04:08","guid":{"rendered":"https:\/\/www.g-strata.com\/?page_id=1171"},"modified":"2026-01-23T12:33:26","modified_gmt":"2026-01-23T15:33:26","slug":"ensayo-de-polarizacion-inducida-de-alta-densidad","status":"publish","type":"page","link":"https:\/\/www.g-strata.com\/en\/ensayo-de-polarizacion-inducida-de-alta-densidad\/","title":{"rendered":"Ensayo de Polarizaci\u00f3n Inducida de Alta Densidad"},"content":{"rendered":"<div data-elementor-type=\"wp-page\" data-elementor-id=\"1171\" class=\"elementor elementor-1171\">\n\t\t\t\t<div class=\"elementor-element elementor-element-c52c747 e-flex e-con-boxed e-con e-parent\" data-id=\"c52c747\" data-element_type=\"container\" data-settings=\"{&quot;background_background&quot;:&quot;classic&quot;}\">\n\t\t\t\t\t<div class=\"e-con-inner\">\n\t\t\t\t<div class=\"elementor-element elementor-element-70288e7 elementor-widget elementor-widget-heading\" data-id=\"70288e7\" data-element_type=\"widget\" data-widget_type=\"heading.default\">\n\t\t\t\t\t<h2 class=\"elementor-heading-title elementor-size-default\">Ensayo de Polarizaci\u00f3n Inducida de Alta Densidad<\/h2>\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t<div class=\"elementor-element elementor-element-bfb1f09 e-flex e-con-boxed e-con e-parent\" data-id=\"bfb1f09\" data-element_type=\"container\">\n\t\t\t\t\t<div class=\"e-con-inner\">\n\t\t<div class=\"elementor-element elementor-element-00791da e-con-full e-flex e-con e-child\" data-id=\"00791da\" data-element_type=\"container\">\n\t\t\t\t<div class=\"elementor-element elementor-element-81e0523 elementor-widget elementor-widget-image\" data-id=\"81e0523\" data-element_type=\"widget\" data-widget_type=\"image.default\">\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<img fetchpriority=\"high\" decoding=\"async\" width=\"620\" height=\"670\" src=\"https:\/\/www.g-strata.com\/wp-content\/uploads\/2026\/01\/5.jpg\" class=\"attachment-large size-large wp-image-1366\" alt=\"\" srcset=\"https:\/\/www.g-strata.com\/wp-content\/uploads\/2026\/01\/5.jpg 620w, https:\/\/www.g-strata.com\/wp-content\/uploads\/2026\/01\/5-278x300.jpg 278w, https:\/\/www.g-strata.com\/wp-content\/uploads\/2026\/01\/5-11x12.jpg 11w\" sizes=\"(max-width: 620px) 100vw, 620px\" \/>\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t<div class=\"elementor-element elementor-element-ca9c02e e-con-full e-flex e-con e-child\" data-id=\"ca9c02e\" data-element_type=\"container\">\n\t\t\t\t<div class=\"elementor-element elementor-element-7b99038 elementor-widget elementor-widget-text-editor\" data-id=\"7b99038\" data-element_type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t\t\t\t\t\t<p>El m\u00e9todo de Polarizaci\u00f3n Inducida (IP) es una t\u00e9cnica geof\u00edsica ampliamente utilizada en exploraci\u00f3n minera y estudios del subsuelo. Su objetivo principal es identificar variaciones en la cargabilidad el\u00e9ctrica de los materiales, lo que permite reconocer zonas asociadas a la presencia de sulfuros met\u00e1licos, arcillas u otros cuerpos mineralizados.<\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-f5af8c9 elementor-widget elementor-widget-text-editor\" data-id=\"f5af8c9\" data-element_type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t\t\t\t\t\t<p><strong>Working Principle:<\/strong><br \/>El m\u00e9todo IP se basa en la inyecci\u00f3n de una corriente el\u00e9ctrica en el terreno y en la medici\u00f3n de la respuesta retardada del subsuelo una vez que la corriente es interrumpida. Esta respuesta se debe al almacenamiento temporal de carga el\u00e9ctrica en los materiales, lo que permite diferenciar sectores con caracter\u00edsticas mineral\u00f3gicas contrastantes y correlacionar anomal\u00edas de resistividad con posibles zonas mineralizadas.<\/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\t\t<\/div>\n\t\t\t\t<\/div>","protected":false},"excerpt":{"rendered":"<p>Ensayo de Polarizaci\u00f3n Inducida de Alta Densidad El m\u00e9todo de Polarizaci\u00f3n Inducida (IP) es una t\u00e9cnica geof\u00edsica ampliamente utilizada en exploraci\u00f3n minera y estudios del subsuelo. Su objetivo principal es identificar variaciones en la cargabilidad el\u00e9ctrica de los materiales, lo que permite reconocer zonas asociadas a la presencia de sulfuros met\u00e1licos, arcillas u otros cuerpos [&hellip;]<\/p>","protected":false},"author":1,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_acf_changed":false,"footnotes":""},"class_list":["post-1171","page","type-page","status-publish","hentry"],"acf":[],"_links":{"self":[{"href":"https:\/\/www.g-strata.com\/en\/wp-json\/wp\/v2\/pages\/1171","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.g-strata.com\/en\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/www.g-strata.com\/en\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/www.g-strata.com\/en\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.g-strata.com\/en\/wp-json\/wp\/v2\/comments?post=1171"}],"version-history":[{"count":7,"href":"https:\/\/www.g-strata.com\/en\/wp-json\/wp\/v2\/pages\/1171\/revisions"}],"predecessor-version":[{"id":1377,"href":"https:\/\/www.g-strata.com\/en\/wp-json\/wp\/v2\/pages\/1171\/revisions\/1377"}],"wp:attachment":[{"href":"https:\/\/www.g-strata.com\/en\/wp-json\/wp\/v2\/media?parent=1171"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}