{"id":48035,"date":"2020-07-30T07:26:39","date_gmt":"2020-07-30T07:26:39","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/el-cretacico-inferior-de-la-region-noroccidental-de-la-provincia-de-valencia\/"},"modified":"2020-07-30T07:26:39","modified_gmt":"2020-07-30T07:26:39","slug":"el-cretacico-inferior-de-la-region-noroccidental-de-la-provincia-de-valencia","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/el-cretacico-inferior-de-la-region-noroccidental-de-la-provincia-de-valencia\/","title":{"rendered":"El cretacico inferior de la region noroccidental de la provincia de Valencia"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Jos\u00e9 Ram\u00f3n Mas Mayoral <\/strong><\/h2>\n<p>Se estudia el cretacico inferior que aflora en la region nw de la provincia de Valencia dentro del sector Valenciano del sistema iberico suroccidental. En estos materiales se han diferenciado 18 unidades litoestratigraficas con diferentes rangos (3 grupos  12 formaciones y 3 miembros). Su estudio bioestratigrafico nos ha permitido identificar sus posiciones cronoestratigraficas  estando representado desde un valanginiense\/hanteriviense hasta un cenomanense inferior. El analisis sedimentologico de estas unidades nos ha permitido reconocer sus facies  que se agrupan en asociaciones representando desde ambientes continentales fluviales hasta ambientes de plataforma interna carbonatada. La integracion de las conclusiones de indole estatrigrafico  sedimentologico y paleogeografico  pone en evidencia que la sedimentacion durante el cretacico inferior en esta region se desarrollo en 6 ciclos sedimentarios separados por discontinuidades estratigraficas (lagunas estratigraficas e hiatos).<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>El cretacico inferior de la region noroccidental de la provincia de Valencia<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 El cretacico inferior de la region noroccidental de la provincia de Valencia <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Jos\u00e9 Ram\u00f3n Mas Mayoral <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Complutense de Madrid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1981<\/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>Carmina Virgili Rodon<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Carmina Virgili Rodon <\/li>\n<li>Pierre Rat (vocal)<\/li>\n<li>Bermudo Melendez Melendez (vocal)<\/li>\n<li> Sanchez De La Torre  Luis (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Jos\u00e9 Ram\u00f3n Mas Mayoral Se estudia el cretacico inferior que aflora en la region nw de la [&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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