{"id":24399,"date":"2003-07-07T00:00:00","date_gmt":"2003-07-07T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/dinamica-ecosedimentaria-durante-el-oxfordiense-medio-kimmeridgiense-temprano-en-la-zona-prebetica-interpretacion-ecoestratigrafica-y-secuencial\/"},"modified":"2003-07-07T00:00:00","modified_gmt":"2003-07-07T00:00:00","slug":"dinamica-ecosedimentaria-durante-el-oxfordiense-medio-kimmeridgiense-temprano-en-la-zona-prebetica-interpretacion-ecoestratigrafica-y-secuencial","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/estratigrafia\/dinamica-ecosedimentaria-durante-el-oxfordiense-medio-kimmeridgiense-temprano-en-la-zona-prebetica-interpretacion-ecoestratigrafica-y-secuencial\/","title":{"rendered":"Dinamica ecosedimentaria durante el oxfordiense medio-kimmeridgiense temprano en la zona prebetica: interpretaci\u00f3n ecoestratigrafica y secuencial"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Matias Reolid P\u00e9rez <\/strong><\/h2>\n<p>Esta investigaci\u00f3n profundiza en el conocimiento de la plataforma epicontinental desarrollada en el margen sudib\u00e9rico durante el intervalo oxfordiense medio-kimmeridgiense temprano (jur\u00e1sico superior), a partir del estudio de los materiales registrados en la zona preb\u00e9tica (cordillera b\u00e9tica). El resultado final se fundamenta en la consecucci\u00f3n de unos objetivos parciales cuyos resultados han sido los siguientes:  1,- el an\u00e1lisis de las microfacies y del estudio macrosc\u00f3pico de los materiales, ha permitido la caracterizaci\u00f3n de cinco grupos de liltofacies: litofacies grumosas, litofacies espongiol\u00edticas, litofacies de ritmita margoso-calc\u00e1rea, litofacies de mangas y litofacies de caliza con oolitos ferruginosos.  2,- el estudio detallado de los carbonatos de origen microbiano ha permtidio clasificar las microbialitas tanto desde el punto de vista microsc\u00f3pico como microsc\u00f3pico. La microbialita tiene un papel fundamental en la formaci\u00f3n de las bioconstrucciones. Se han reconocido bioconstrucciones simples y complejas, constituidas por una fase de biohermo de esponjas y una fase de litohermo microbiano.  3,- el an\u00e1lisis de las asociaciones de foramin\u00edferos, su distribuci\u00f3n y relaci\u00f3n con las litofacies ha permitido diferenciar una asociaci\u00f3n relativamente proximal (preb\u00e9tico externo) de otra m\u00e1s distal (preb\u00e9tico interno).  4,- la bioestratigrafia a nivel de zona se ha basado en el an\u00e1lisis de los ammonoideos, reconociendo desde la zona transversarium (oxfordiense medio) a la zona platynota (kimmeridgiense inferior).  5,- se ha realizado un estudio tafon\u00f3mico de los macroinvertebrados f\u00f3siles registrados, centrado en: modalidad de conservaci\u00f3n, tama\u00f1o de los ejemplares, posici\u00f3n en el estrato, \u00abcorrasion\u00bb, fragmentaci\u00f3n, epibiontes y encostramientos, desarticulaci\u00f3n, desacoplamiento, facetado y deformaci\u00f3n. se han diferenciado cuatro tafofacies, i, ii, iii y iv.  6,- el an\u00e1lisis de la composici\u00f3n de la<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Dinamica ecosedimentaria durante el oxfordiense medio-kimmeridgiense temprano en la zona prebetica: interpretaci\u00f3n ecoestratigrafica y secuencial<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Dinamica ecosedimentaria durante el oxfordiense medio-kimmeridgiense temprano en la zona prebetica: interpretaci\u00f3n ecoestratigrafica y secuencial <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Matias Reolid P\u00e9rez <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Granada<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 07\/07\/2003<\/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>Federico Oloriz Saez<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal:  L\u00f3pez garrido angel Carlos <\/li>\n<li>concepci\u00f3n Herreo matesanz (vocal)<\/li>\n<li>christian Gaillard (vocal)<\/li>\n<li> Tavera benitez Jos\u00e9 Mar\u00eda (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Matias Reolid P\u00e9rez Esta investigaci\u00f3n profundiza en el conocimiento de la plataforma epicontinental desarrollada en el margen [&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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