{"id":1181,"date":"2026-01-22T20:08:19","date_gmt":"2026-01-22T23:08:19","guid":{"rendered":"https:\/\/www.g-strata.com\/?page_id=1181"},"modified":"2026-01-23T12:33:59","modified_gmt":"2026-01-23T15:33:59","slug":"metodo-de-refraccion-sismica","status":"publish","type":"page","link":"https:\/\/www.g-strata.com\/en\/metodo-de-refraccion-sismica\/","title":{"rendered":"M\u00e9todo de Refracci\u00f3n S\u00edsmica"},"content":{"rendered":"<div data-elementor-type=\"wp-page\" data-elementor-id=\"1181\" class=\"elementor elementor-1181\">\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\">M\u00e9todo de Refracci\u00f3n S\u00edsmica<\/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-b45295f elementor-widget elementor-widget-image\" data-id=\"b45295f\" 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\/7.jpg\" class=\"attachment-large size-large wp-image-1369\" alt=\"\" srcset=\"https:\/\/www.g-strata.com\/wp-content\/uploads\/2026\/01\/7.jpg 620w, https:\/\/www.g-strata.com\/wp-content\/uploads\/2026\/01\/7-278x300.jpg 278w, https:\/\/www.g-strata.com\/wp-content\/uploads\/2026\/01\/7-11x12.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 refracci\u00f3n s\u00edsmica es una t\u00e9cnica geof\u00edsica ampliamente utilizada<br \/>para determinar la velocidad de propagaci\u00f3n de las ondas s\u00edsmicas compresionales en el subsuelo (Vp), lo que permite caracterizar las capas geol\u00f3gicas y estructuras subsuperficiales. Este m\u00e9todo<br \/>es valioso para la ingenier\u00eda geot\u00e9cnica, la exploraci\u00f3n de recursos naturales, la planificaci\u00f3n de proyectos de construcci\u00f3n y ripabilidad del terreno.<\/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 de refracci\u00f3n s\u00edsmica se basa en el tiempo que tardan las ondas s\u00edsmicas en<br \/>viajar desde una fuente s\u00edsmica en la superficie hasta los receptores o ge\u00f3fonos ubicados en diferentes distancias a lo largo de un tendido o l\u00ednea s\u00edsmica. La variaci\u00f3n de las velocidades de propagaci\u00f3n de las ondas en diferentes capas del subsuelo se utiliza para inferir las caracter\u00edsticas geol\u00f3gicas.<\/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>M\u00e9todo de Refracci\u00f3n S\u00edsmica El m\u00e9todo de refracci\u00f3n s\u00edsmica es una t\u00e9cnica geof\u00edsica ampliamente utilizadapara determinar la velocidad de propagaci\u00f3n de las ondas s\u00edsmicas compresionales en el subsuelo (Vp), lo que permite caracterizar las capas geol\u00f3gicas y estructuras subsuperficiales. Este m\u00e9todoes valioso para la ingenier\u00eda geot\u00e9cnica, la exploraci\u00f3n de recursos naturales, la planificaci\u00f3n de proyectos [&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-1181","page","type-page","status-publish","hentry"],"acf":[],"_links":{"self":[{"href":"https:\/\/www.g-strata.com\/en\/wp-json\/wp\/v2\/pages\/1181","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=1181"}],"version-history":[{"count":7,"href":"https:\/\/www.g-strata.com\/en\/wp-json\/wp\/v2\/pages\/1181\/revisions"}],"predecessor-version":[{"id":1383,"href":"https:\/\/www.g-strata.com\/en\/wp-json\/wp\/v2\/pages\/1181\/revisions\/1383"}],"wp:attachment":[{"href":"https:\/\/www.g-strata.com\/en\/wp-json\/wp\/v2\/media?parent=1181"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}