{"id":2003,"date":"2021-07-14T12:20:49","date_gmt":"2021-07-14T12:20:49","guid":{"rendered":"https:\/\/www.igeotest.ad\/geo-3\/"},"modified":"2022-04-14T09:04:21","modified_gmt":"2022-04-14T09:04:21","slug":"geo-3","status":"publish","type":"page","link":"https:\/\/www.igeotest.ad\/es\/geo-3\/","title":{"rendered":"GEO 3"},"content":{"rendered":"[vc_row][vc_column][vc_column_text]<span style=\"color: #800000;\"><strong>PROSPECCI\u00d3N GEOF\u00cdSICA Y CARTOGRAF\u00cdA TEM\u00c1TICA<\/strong><\/span><\/p>\n<p>Para el estudio del subsuelo se puede recurrir a m\u00e9todos de prospecci\u00f3n directos y\/o indirectos. Los m\u00e9todos directos (sondeos mec\u00e1nicos, catas mec\u00e1nicas, etc&#8230;), pueden dar una informaci\u00f3n de buena resoluci\u00f3n pero puntual, mientras que los m\u00e9todos indirectos (sondeos el\u00e9ctricos verticales, s\u00edsmica de refracci\u00f3n, calicatas el\u00e9ctricas, etc&#8230;), pueden dar una informaci\u00f3n m\u00e1s extensa pero con menos resoluci\u00f3n. A menudo la combinaci\u00f3n de los m\u00e9todos directos e indirectos generan un buen resultado, desde el punto de vista calidad\/precio\/tiempo.<\/p>\n<p>&nbsp;[\/vc_column_text][vc_row_inner][vc_column_inner width=\u00bb1\/2&#8243;][vc_single_image image=\u00bb2006&#8243; alignment=\u00bbcenter\u00bb][\/vc_column_inner][vc_column_inner width=\u00bb1\/2&#8243;][vc_single_image image=\u00bb2010&#8243; alignment=\u00bbcenter\u00bb][\/vc_column_inner][\/vc_row_inner][vc_column_text]Llevamos desde el a\u00f1o 1994 desarrollando la combinaci\u00f3n de los m\u00e9todos directos e indirectos con <a href=\"https:\/\/sites.google.com\/site\/geoternasl\/\" target=\"_blank\" rel=\"noopener\">GEOTERNA Ge\u00f2legs Consultors<\/a>.<\/p>\n<p>&nbsp;[\/vc_column_text][vc_row_inner][vc_column_inner width=\u00bb1\/3&#8243;][\/vc_column_inner][vc_column_inner width=\u00bb1\/3&#8243;][vc_single_image image=\u00bb2015&#8243; alignment=\u00bbcenter\u00bb][\/vc_column_inner][vc_column_inner width=\u00bb1\/3&#8243;][\/vc_column_inner][\/vc_row_inner][vc_row_inner][vc_column_inner width=\u00bb1\/3&#8243;][vc_single_image image=\u00bb1280&#8243; alignment=\u00bbcenter\u00bb][\/vc_column_inner][vc_column_inner width=\u00bb1\/3&#8243;][vc_single_image image=\u00bb1283&#8243; alignment=\u00bbcenter\u00bb][\/vc_column_inner][vc_column_inner width=\u00bb1\/3&#8243;][vc_single_image image=\u00bb1286&#8243; alignment=\u00bbcenter\u00bb][\/vc_column_inner][\/vc_row_inner][vc_row_inner][vc_column_inner width=\u00bb1\/6&#8243;][\/vc_column_inner][vc_column_inner width=\u00bb2\/3&#8243;][vc_column_text]\n<p style=\"text-align: center;\">Somos distribuidores autorizados de <a href=\"http:\/\/www.zzgeo.com\/\" target=\"_blank\" rel=\"noopener\">ZZ Resistivity Imaging Pty. Ltd<\/a>.<\/p>\n[\/vc_column_text][vc_video link=\u00bbhttps:\/\/www.youtube.com\/watch?v=HKPPWfE-aMg\u00bb][\/vc_column_inner][vc_column_inner width=\u00bb1\/6&#8243;][\/vc_column_inner][\/vc_row_inner][\/vc_column][\/vc_row][vc_row][vc_column][vc_separator][\/vc_column][\/vc_row]\n","protected":false},"excerpt":{"rendered":"<p>[vc_row][vc_column][vc_column_text]PROSPECCI\u00d3N GEOF\u00cdSICA Y CARTOGRAF\u00cdA TEM\u00c1TICA Para el estudio del subsuelo se puede recurrir a m\u00e9todos de prospecci\u00f3n directos y\/o indirectos. Los m\u00e9todos directos (sondeos mec\u00e1nicos, catas mec\u00e1nicas, etc&#8230;), pueden dar una informaci\u00f3n de buena resoluci\u00f3n pero puntual, mientras que los&hellip;<\/p>\n","protected":false},"author":2,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":[],"_links":{"self":[{"href":"https:\/\/www.igeotest.ad\/es\/wp-json\/wp\/v2\/pages\/2003"}],"collection":[{"href":"https:\/\/www.igeotest.ad\/es\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/www.igeotest.ad\/es\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/www.igeotest.ad\/es\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/www.igeotest.ad\/es\/wp-json\/wp\/v2\/comments?post=2003"}],"version-history":[{"count":7,"href":"https:\/\/www.igeotest.ad\/es\/wp-json\/wp\/v2\/pages\/2003\/revisions"}],"predecessor-version":[{"id":2023,"href":"https:\/\/www.igeotest.ad\/es\/wp-json\/wp\/v2\/pages\/2003\/revisions\/2023"}],"wp:attachment":[{"href":"https:\/\/www.igeotest.ad\/es\/wp-json\/wp\/v2\/media?parent=2003"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}