{"id":49746,"date":"2021-05-08T18:19:17","date_gmt":"2021-05-08T18:19:17","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/el-complejo-esquisto-grauvaquico-las-series-paleozoicas-y-la-estructura-hercinica-al-sur-de-salamanca\/"},"modified":"2021-05-08T18:19:17","modified_gmt":"2021-05-08T18:19:17","slug":"el-complejo-esquisto-grauvaquico-las-series-paleozoicas-y-la-estructura-hercinica-al-sur-de-salamanca","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/el-complejo-esquisto-grauvaquico-las-series-paleozoicas-y-la-estructura-hercinica-al-sur-de-salamanca\/","title":{"rendered":"El complejo esquisto-grauvaquico, las series paleozoicas y la estructura hercinica al sur de salamanca."},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Diez Balda M. Antonia <\/strong><\/h2>\n<p>Se presenta un trabajo de geolog\u00eda regional que comprende aproximadamente el cuadrante sureste de la provincia de salamanca. La cartografia geologica de este area a escala 1:200.000 acompa\u00f1a a la memoria. Los materiales que afloran en esta region (pertenecientes al complejo esquisto grauvaquico  alcambrico inferior  alordovicico y alsilurico) fueron deformacion. La primera origino grandes pliegues de direccion nw-se  verticales acompa\u00f1ados de una esquistosidad s1. La segunda fase produjo pliegues de plano axial horizontal acompa\u00f1ados de una esquistosidad horizontal s2 y superficies de cizalla subhorizontales. La tercera fase produjo suaves antiformas y sinformas de direccion e-w verticales. Se estudian las estructuras de cada fase su geometria y distribucion en el corte. Se interpreta la estructura general y se aportan conclusiones tanto sobre la estratigrafia como sobre la tectonica.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>El complejo esquisto-grauvaquico, las series paleozoicas y la estructura hercinica al sur de salamanca.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 El complejo esquisto-grauvaquico, las series paleozoicas y la estructura hercinica al sur de salamanca. <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Diez Balda M. Antonia <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Salamanca<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1982<\/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>Florencio Aldaya Valverde<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Carlos Garcia Figuerola <\/li>\n<li>Enrique Mart\u00ednez Garc\u00eda (vocal)<\/li>\n<li>Florencio Aldaya Valverde (vocal)<\/li>\n<li>Ram\u00f3n Vegas Mart\u00ednez (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Diez Balda M. Antonia Se presenta un trabajo de geolog\u00eda regional que comprende aproximadamente el cuadrante sureste [&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":[27,953,3435,9386],"tags":[37747,75783,9532,3439,46267],"class_list":["post-49746","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-tierra-y-del-espacio","category-geologia","category-geologia-estructural","category-salamanca","tag-carlos-garcia-figuerola","tag-diez-balda-m-antonia","tag-enrique-Martinez-garcia","tag-florencio-aldaya-valverde","tag-ramon-vegas-Martinez"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/49746","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=49746"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/49746\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=49746"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=49746"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=49746"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}