{"id":137229,"date":"2026-01-12T17:03:50","date_gmt":"2026-01-12T17:03:50","guid":{"rendered":""},"modified":"2026-01-12T17:03:50","modified_gmt":"2026-01-12T17:03:50","slug":"estudio-geologico-estructural-de-los-materiales-precambricos-y-paleozoicos-entre-la-sierra-de-san-pedro-y-la-depresion-del-guadiana-provincia-de-caceres-y-badajoz-sector-limite-entre-las-zonas-cent","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/estudio-geologico-estructural-de-los-materiales-precambricos-y-paleozoicos-entre-la-sierra-de-san-pedro-y-la-depresion-del-guadiana-provincia-de-caceres-y-badajoz-sector-limite-entre-las-zonas-cent\/","title":{"rendered":"Estudio geologico-estructural de los materiales precambricos y paleozoicos entre la sierra de san pedro y la depresion del guadiana (provincia de caceres y badajoz). sector limite entre las zonas centroiberica y ossa-morena."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Juan Soldevila Bartoli <\/strong><\/h2>\n<p>Se describen las caracteristicas litologicas y estructurales de los materiales precambricos y paleozoicos que se extienden entre la sierra de san pedro y la depresion del guadiana, en la zona limitrofe entre las provincias de caceres y badajoz. El area estudiada se situa sobre la parte meridional de la zona centroiberica y a lo largo de su limite con la zona de ossa-morena. Se establecen cinco dominios atendiendo a las caracteristicas litologicas y estructurales, de los cuales el situado mas al s (dominio v) presenta caracteristicas que permiten correlacionarlo con los materiales precambricos de la zona de ossa-morena, mientras los restantes pueden correlacionarse con materiales paleozoicos y precambricos de la zona centroiberica. Se establece el cabalgamiento de la zona de ossa-morena sobre la centroiberica en este sector. Se describen las caracteristicas del metamorfismo regional y de contacto en la region, y se caracterizan composicionalmente las rocas igneas, de las que se diferencian diversos grupos atendiendo a su afloramiento y a sus relaciones con la deformacion.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Estudio geologico-estructural de los materiales precambricos y paleozoicos entre la sierra de san pedro y la depresion del guadiana (provincia de caceres y badajoz). sector limite entre las zonas centroiberica y ossa-morena.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Estudio geologico-estructural de los materiales precambricos y paleozoicos entre la sierra de san pedro y la depresion del guadiana (provincia de caceres y badajoz). sector limite entre las zonas centroiberica y ossa-morena. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Juan Soldevila Bartoli <\/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\/1991<\/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>Manuel Julivert Casagualda<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Pere Santanach Prat <\/li>\n<li>Ram\u00f3n Vegas Mart\u00ednez (vocal)<\/li>\n<li>Jordi Carreras Planells (vocal)<\/li>\n<li>Francisco Sabat Montserrat (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Juan Soldevila Bartoli Se describen las caracteristicas litologicas y estructurales de los materiales precambricos y paleozoicos que [&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 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