{"id":131130,"date":"1996-01-01T00:00:00","date_gmt":"1996-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/los-yacimientos-de-fosfato-sedimentario-en-el-limite-precambrico-cambrico-del-anticlinal-de-valdelacasa-zona-centro-iberica\/"},"modified":"1996-01-01T00:00:00","modified_gmt":"1996-01-01T00:00:00","slug":"los-yacimientos-de-fosfato-sedimentario-en-el-limite-precambrico-cambrico-del-anticlinal-de-valdelacasa-zona-centro-iberica","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/los-yacimientos-de-fosfato-sedimentario-en-el-limite-precambrico-cambrico-del-anticlinal-de-valdelacasa-zona-centro-iberica\/","title":{"rendered":"Los yacimientos de fosfato sedimentario en el limite precambrico-cambrico del anticlinal de valdelacasa (zona centro-iberica)."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Joan Santamaria Casanovas <\/strong><\/h2>\n<p>En primer lugar se realiza la jerarquizacion estratigrafica de los materiales precambrico-cambrico del anticlinal de valdelacasa, junto con su interpretacion sedimentologica. Se integra la evolucion de estos materiales dentro del contexto de la tectonica de placas avalonio-cadoniense, se situan los diversos indicios de fosfato encontrados.  la segunda parte trata en profundidad de los yacimientos de fosforos encontrados en el area de estudio, tanto desde el punto de vista estratigrafico y sedimentologico como geoquimico y petrologico, dando una hipotesis sobre su formacion en origen y posterior retrabajamiento y acumulacion= yacimiento.  en anexos se pretende una cartografia del area estudiada, y evolucion de los conocimientos sobre los fosfatos sedimentarios.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Los yacimientos de fosfato sedimentario en el limite precambrico-cambrico del anticlinal de valdelacasa (zona centro-iberica).<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Los yacimientos de fosfato sedimentario en el limite precambrico-cambrico del anticlinal de valdelacasa (zona centro-iberica). <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Joan Santamaria Casanovas <\/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\/1996<\/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>Eduard Remacha Grau<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Joan Rosell Sanuy <\/li>\n<li> Suarez De Centi Cesar (vocal)<\/li>\n<li>Ram\u00f3n Salas Roig (vocal)<\/li>\n<li>Joan Carles Melgarejo Draper (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Joan Santamaria Casanovas En primer lugar se realiza la jerarquizacion estratigrafica de los materiales precambrico-cambrico del anticlinal [&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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