{"id":14768,"date":"2018-03-09T09:01:36","date_gmt":"2018-03-09T09:01:36","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/estudio-geofisico-de-una-cuenca-sedimentaria-la-cuenca-de-almazan-provincia-de-soria-implicaciones-tectonicas\/"},"modified":"2018-03-09T09:01:36","modified_gmt":"2018-03-09T09:01:36","slug":"estudio-geofisico-de-una-cuenca-sedimentaria-la-cuenca-de-almazan-provincia-de-soria-implicaciones-tectonicas","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/estudio-geofisico-de-una-cuenca-sedimentaria-la-cuenca-de-almazan-provincia-de-soria-implicaciones-tectonicas\/","title":{"rendered":"Estudio geofisico de una cuenca sedimentaria: la cuenca de almazan (provincia de soria). implicaciones tectonicas"},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Rey Moral M. Carmen <\/strong><\/h2>\n<p>La cuenca de almazan es una cuenca sedimentaria rellena de materiales terciarios de car\u00e1cter continental. Contituye la zona oriental de la cuenca del duero y forma parte del area noroccidental de la cordillera iberica. La investigacion tiene como objeto principal el estudio de la estructura de la corteza de la cuenca, para lo cual se han utilizado metodos sismicos y gravimetricos. a partir de la restitucion de los perfiles sismicos de reflexion disponibles se ha obtenido la geometria profunda de la cuenca. La realizacion del levantamieto gravimetrico de la region, la elaboracion de una mapa de anomalias de bouguer a partir de los datos obtenidos y las medidas de densidad han permitido calcular las profundidades de las fuentes que generan las anomalias gravimetricas y realizar modelos de densidades de la estructura de la corteza. La integracion de datos geologicos y geofisicos han limitado los posibles modelos que satisfacen las anomalias gravimetricas. La estructura resultante muestra la existencia de una elevacion de la superficie de moho y la geometria domica de los limites de las capas corticales bajo la cuenca de almazan. el significado de esta estructura cortical se ha analizado estudiando la relacion con la topografia y con la tectonica de la zona, concluyendo que el domo cortical es consecuencia del regimen extensional que ha dominado el ne peninsular desde el mioceno superior.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Estudio geofisico de una cuenca sedimentaria: la cuenca de almazan (provincia de soria). implicaciones tectonicas<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Estudio geofisico de una cuenca sedimentaria: la cuenca de almazan (provincia de soria). implicaciones tectonicas <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Rey Moral M. Carmen <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Complutense de Madrid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 19\/12\/2001<\/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>Rosa Mar\u00eda Tejero L\u00f3pez<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: ramon Capote del villar <\/li>\n<li>Juan  Luis Plata torres (vocal)<\/li>\n<li>Jos\u00e9 ram\u00f3n Mas mayoral (vocal)<\/li>\n<li>Fernando Alvarez lobato (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Rey Moral M. Carmen La cuenca de almazan es una cuenca sedimentaria rellena de materiales terciarios de [&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":[27,1033,20496],"tags":[45212,22058,47404,6703,47402,47403],"class_list":["post-14768","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-tierra-y-del-espacio","category-geofisica","category-tectonica","tag-fernando-alvarez-lobato","tag-jose-ramon-mas-mayoral","tag-juan-luis-plata-torres","tag-ramon-capote-del-villar","tag-rey-moral-m-carmen","tag-rosa-maria-tejero-lopez"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/14768","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=14768"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/14768\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=14768"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=14768"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=14768"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}