{"id":140611,"date":"2026-01-12T17:56:10","date_gmt":"2026-01-12T17:56:10","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/analisis-geologico-de-la-cuenca-colima-jalisco-y-su-relacion-con-cuencas-limitrofes-sector-sudoccidental-de-mexico\/"},"modified":"2026-01-12T17:56:10","modified_gmt":"2026-01-12T17:56:10","slug":"analisis-geologico-de-la-cuenca-colima-jalisco-y-su-relacion-con-cuencas-limitrofes-sector-sudoccidental-de-mexico","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/analisis-geologico-de-la-cuenca-colima-jalisco-y-su-relacion-con-cuencas-limitrofes-sector-sudoccidental-de-mexico\/","title":{"rendered":"Analisis geologico de la cuenca colima-jalisco y su relacion con cuencas limitrofes (sector sudoccidental de mexico)"},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Barba Lopez Isabel M. <\/strong><\/h2>\n<p>Se define el complejo metamorfico que conforma el zocalo de la cuenca colima-jalisco, como constituido por tres unidades: migmatitas las juntas (facies anfibolitica con una edad de recalentamiento de 287 + 23 m.A); metasedimentos cerro prieto y metasedimentos arteaga (facies de esquistos verdes de edad triasico tardio, metamorfizada en el jurasico temprano 189 + m.A). En su conjunto, este zocalo es correlacionable con el complejo xolapa de la cuenca guerrero-morelos. La corbetera sedimentaria (jurasico superior-cenomaniano inferior) esta representada por las formaciones tecalitlan, alberca (miembro de la anterior formacion), telpalcatepec y Madrid, cuyo origen es el resultado de la evolucion de un arco volcanico de margen continental  de direccion nw-se que migra en tiempo de sw a ne. La distribucion de litofacies de estas formaciones evidencia una afinidad pacifica y no del golfo de mexico. Todas estas formaciones son correlacionables con las unidades presentes en las cuencas de michoacan y guerrero morelos.  la estructura actual de la cuenca colima-jalisco es resultado del desplazamiento de bloques en sentido sw-ne y nw-se asociado a la fase orogenica sevier y al evento laramidico que desplazo el \u00abbloque chortis\u00bb.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Analisis geologico de la cuenca colima-jalisco y su relacion con cuencas limitrofes (sector sudoccidental de mexico)<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Analisis geologico de la cuenca colima-jalisco y su relacion con cuencas limitrofes (sector sudoccidental de mexico) <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Barba Lopez Isabel M. <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Aut\u00f3noma de barcelona<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1992<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n<h3>Direcci\u00f3n y tribunal<\/h3>\n<ul>\n<li><strong>Director de la tesis<\/strong>\n<ul>\n<li>Josep Trilla Arrufat<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Emilio Elizaga Mu\u00f1oz <\/li>\n<li>Joan Rosell Sanuy (vocal)<\/li>\n<li>Jos\u00e9 Antonio Ageda Villar (vocal)<\/li>\n<li>Sergio Robles Orozco (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Barba Lopez Isabel M. Se define el complejo metamorfico que conforma el zocalo de la cuenca colima-jalisco, [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"site-sidebar-layout":"default","site-content-layout":"","ast-site-content-layout":"","site-content-style":"default","site-sidebar-style":"default","ast-global-header-display":"","ast-banner-title-visibility":"","ast-main-header-display":"","ast-hfb-above-header-display":"","ast-hfb-below-header-display":"","ast-hfb-mobile-header-display":"","site-post-title":"","ast-breadcrumbs-content":"","ast-featured-img":"","footer-sml-layout":"","theme-transparent-header-meta":"","adv-header-id-meta":"","stick-header-meta":"","header-above-stick-meta":"","header-main-stick-meta":"","header-below-stick-meta":"","astra-migrate-meta-layouts":"default","ast-page-background-enabled":"default","ast-page-background-meta":{"desktop":{"background-color":"var(--ast-global-color-4)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"ast-content-background-meta":{"desktop":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"footnotes":""},"categories":[27,953,19202],"tags":[255244,254009,46550,255245,87232,13246],"class_list":["post-140611","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-tierra-y-del-espacio","category-geologia","category-geologia-regional","tag-barba-lopez-isabel-m","tag-emilio-elizaga-munoz","tag-joan-rosell-sanuy","tag-jose-antonio-ageda-villar","tag-josep-trilla-arrufat","tag-sergio-robles-orozco"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/140611","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/comments?post=140611"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/140611\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=140611"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=140611"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=140611"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}