{"id":38597,"date":"2018-03-09T09:38:14","date_gmt":"2018-03-09T09:38:14","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/les-evaporites-de-les-conques-betiques-marginals-fortuna-lorca-mioce-superior-comparacio-amb-altres-conques-mediterranies\/"},"modified":"2018-03-09T09:38:14","modified_gmt":"2018-03-09T09:38:14","slug":"les-evaporites-de-les-conques-betiques-marginals-fortuna-lorca-mioce-superior-comparacio-amb-altres-conques-mediterranies","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/les-evaporites-de-les-conques-betiques-marginals-fortuna-lorca-mioce-superior-comparacio-amb-altres-conques-mediterranies\/","title":{"rendered":"Les evaporites de les conques betiques marginals (fortuna-lorca, mioce superior): comparacio amb altres conques mediterranies."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Elisabet Playa Pous <\/strong><\/h2>\n<p>Las cuencas ne\u00f3genas de las cordilleras b\u00e9ticas orientales se situaron en posici\u00f3n marginal durante la crisis de salinidad messiniense respecto a la cuenca mediterr\u00e1nea profunda. En el presente trabajo se han estudiado en profundidad las principales cuencas evapor\u00edticas marginales: las cuencas de fortuna, corredor del guadalent\u00edn, archena-mula y lorca. Dentro del contexto de las cordilleras b\u00e9ticas orientales tambi\u00e9n se encuentran algunas cuencas evapor\u00edticas con caracter\u00edsticas m\u00e1s similares a las de la cuenca mediterr\u00e1nea profunda: son las cuencas de sorbas, benej\u00fazar, san miguel de salinas y mallorca. Estas cubetas presentan potentes series de yesos primarios selen\u00edticos, aunque no se conoce la existencia de tramos hal\u00edticos en estas series. La comparaci\u00f3n de estas unidades de yesos con las de las cuencas situadas entre fortuna y lorca, tanto desde el punto de vista petrol\u00f3gico como geoqu\u00edmico, permitir\u00e1 comparar los registros evapor\u00edticos messinienses en las diferentes \u00e1reas paleogeogr\u00e1ficas y profundizar en el conocimiento de la crisis de salinidad messiniense. Adem\u00e1s, tambi\u00e9n se han incluido algunas observaciones de la serie yesos de la cuenca de caltanissetta (sicilia). En el conjunto evapor\u00edtico messiniense de las cuencas entre fortuna y lorca se pueden distinguir varias unidades de yesos que presentan caracter\u00edsticas petrol\u00f3gicas (y geoqu\u00edmicas) propias.  cada una de las diferentes unidades evapor\u00edticas messinienses distinguidas en las cuencas entre fortuna y lorca presentan composiciones isot\u00f3picas particulares y propias, y estas propiedades geoqu\u00edmicas se mantienen invariables. Las composiciones isot\u00f3picas del estroncio soportan las conclusiones obtenidas a partir de los an\u00e1lisis isot\u00f3picos del sulfato, ya que las relaciones 87sr\/86sr muestran una tendencia pr\u00e1cticamente paralela a las composiciones del sulfato.  una vez definidas y descritas las series de yesos de las cuencas de fo<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Les evaporites de les conques betiques marginals (fortuna-lorca, mioce superior): comparacio amb altres conques mediterranies.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Les evaporites de les conques betiques marginals (fortuna-lorca, mioce superior): comparacio amb altres conques mediterranies. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Elisabet Playa Pous <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Barcelona<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 21\/09\/1998<\/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 Orti Cabo<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: francesc Calvet rovira <\/li>\n<li>Jos\u00e9 pedro Calvo sorando (vocal)<\/li>\n<li>rosa Utrilla casal (vocal)<\/li>\n<li>jean marie Rouchy (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Elisabet Playa Pous Las cuencas ne\u00f3genas de las cordilleras b\u00e9ticas orientales se situaron en posici\u00f3n marginal durante [&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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