{"id":5994,"date":"1995-01-01T00:00:00","date_gmt":"1995-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/1995\/01\/01\/el-paleokarst-del-lecho-de-la-unidad-intermedia-del-mioceno-de-la-cuenca-de-madrid\/"},"modified":"1995-01-01T00:00:00","modified_gmt":"1995-01-01T00:00:00","slug":"el-paleokarst-del-lecho-de-la-unidad-intermedia-del-mioceno-de-la-cuenca-de-madrid","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/el-paleokarst-del-lecho-de-la-unidad-intermedia-del-mioceno-de-la-cuenca-de-madrid\/","title":{"rendered":"El paleokarst del lecho de la unidad intermedia del mioceno de la cuenca de Madrid"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Juan  Carlos Ca\u00f1averas  Jimenez <\/strong><\/h2>\n<p>A techo de la unidad intermedia del mioceno de la cuenca de Madrid se reconoce una ruptura sedimentaria de origen paleokarstico. Este paleokarst presenta una gran extension lateral y un escaso espesor, dibujan una geometria tabular. Asimismo se han reconocido una amplia variedad de formas y depositos tanto endokarsticos como exokarsticos, desarrolla sobre materiales carbonaticos y evaporiticos.  el paleokarst representa el primer reflejo en un cambio de regimen sedimentario de la cuenca durante el vallesiense, pasando de unas condiciones endoreicas (u. Intemedia) a condiciones exorreicas (u. Superior), lo que implica una cierta apertura de la cuenca. El desencadenante de esta ruptura es el cambio de regimen tectonico de los bordes de la cuenca, de compresivo a distensivo, cambio que tambien ha sido reconocido en otras cuencas continentales ibericas.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>El paleokarst del lecho de la unidad intermedia del mioceno de la cuenca de Madrid<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 El paleokarst del lecho de la unidad intermedia del mioceno de la cuenca de Madrid <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Juan  Carlos Ca\u00f1averas  Jimenez <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Complutense de Madrid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1995<\/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>Jos\u00e9 Pedro Calvo Sorando<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Manuel Bustillo Revuelta <\/li>\n<li>Mateu Esteban Cerda (vocal)<\/li>\n<li>Luis Pomar  Goma (vocal)<\/li>\n<li> Garcia Del Cura M. Angeles (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Juan Carlos Ca\u00f1averas Jimenez A techo de la unidad intermedia del mioceno de la cuenca de Madrid [&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":[27,953,3857],"tags":[22940,4764,22937,3821,22938,22939],"class_list":["post-5994","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-tierra-y-del-espacio","category-geologia","category-sedimentologia","tag-garcia-del-cura-m-angeles","tag-jose-pedro-calvo-sorando","tag-juan-carlos-canaveras-jimenez","tag-luis-pomar-goma","tag-manuel-bustillo-revuelta","tag-mateu-esteban-cerda"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/5994","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=5994"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/5994\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=5994"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=5994"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=5994"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}