{"id":133085,"date":"1997-01-01T00:00:00","date_gmt":"1997-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/estratigrafia-secuencial-de-sistemas-deltaicos-en-cuencas-de-antepais-ejemplos-de-sant-llorenc-del-munt-montserrat-y-roda\/"},"modified":"1997-01-01T00:00:00","modified_gmt":"1997-01-01T00:00:00","slug":"estratigrafia-secuencial-de-sistemas-deltaicos-en-cuencas-de-antepais-ejemplos-de-sant-llorenc-del-munt-montserrat-y-roda","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/estratigrafia-secuencial-de-sistemas-deltaicos-en-cuencas-de-antepais-ejemplos-de-sant-llorenc-del-munt-montserrat-y-roda\/","title":{"rendered":"Estratigrafia secuencial de sistemas deltaicos en cuencas de antepais: ejemplos de sant llorenc del munt, montserrat y roda."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Miguel Lopez Blanco <\/strong><\/h2>\n<p>Tras el analisis sedimentologico y estratigrafico de los sistemas deltaicos de sant llorenc del munt, montserrat y roda, se ha optado por realizar una subdivision estratigrafica basada en secuencias de tipo transgresivo- regresivo, de tres diferentes escalas. En base al analisis realizado, se ha constatado que existen tres factores principales que controlan la ciclicidad (eustatismo, subsidencia y aportes sedimentarios). En las cuencas de antepais, los factores de control locales (subsidencia y aportes) son variables tanto en el tiempo como en el espacio, lo que hace que las secuencias, en este tipo de cuencas, tengan un valor local de cara a realizar correlaciones. Las secuencias seran correlacionables en sectores en los que los factores de control operen con magnitud y periodicidad similares.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Estratigrafia secuencial de sistemas deltaicos en cuencas de antepais: ejemplos de sant llorenc del munt, montserrat y roda.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Estratigrafia secuencial de sistemas deltaicos en cuencas de antepais: ejemplos de sant llorenc del munt, montserrat y roda. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Miguel Lopez Blanco <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Barcelona<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1997<\/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>Mar\u00eda no Marzo Carpio<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Josep Serra Kiel <\/li>\n<li>Pedro Anadon Monzon (vocal)<\/li>\n<li>Ram\u00f3n Salas Roig (vocal)<\/li>\n<li>Ronald Steel (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Miguel Lopez Blanco Tras el analisis sedimentologico y estratigrafico de los sistemas deltaicos de sant llorenc del [&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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