{"id":20977,"date":"2018-03-09T09:10:32","date_gmt":"2018-03-09T09:10:32","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/estratigrafia-del-eoceno-oligoceno-de-la-cuenca-de-jaca-sinclinorio-de-guarga\/"},"modified":"2018-03-09T09:10:32","modified_gmt":"2018-03-09T09:10:32","slug":"estratigrafia-del-eoceno-oligoceno-de-la-cuenca-de-jaca-sinclinorio-de-guarga","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/estratigrafia-del-eoceno-oligoceno-de-la-cuenca-de-jaca-sinclinorio-de-guarga\/","title":{"rendered":"Estratigrafia del eoceno-oligoceno de la cuenca de jaca (sinclinorio de guarga)"},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Montes Santiago Manuel Jes\u00fas <\/strong><\/h2>\n<p>El sinclinorio del guarga forma parte de la cuenca sinorog\u00e9nica de jaca, situada en la vertiente sur del pirineo central. Los dep\u00f3sitos del sinclinorio (luteciense superior-oligoceno), poseen una gran variedad de facies (marinas y continentales), que han sido plasmadas en una cartograf\u00eda  geol\u00f3gica de s\u00edntesis a escala 1:100.00, obtenida en escalas de trabajo 1:25.000 y 1:50.000.  las relaciones gen\u00e9ticas entre las diversas unidades cartogr\u00e1ficas, dividen el registro sedimentario en una serie de unidades jerarquizadas, limitadas a muro y a techo por discontinuidades y\/o sus continuidades correlativas, siguiendo los postulados de la estrategia secuencial. La cartograf\u00eda de dichas discontinuidades, ha permitido definir de mayor a menor rango: 3 grupos, 7 megasecuencias y 14 secuencias.  las discontinuidades basales de las unidades secuenciales mayores (grupos y megasecuencias), marcan cambios importantes en la distribuci\u00f3n de facies, ambientes sedimentarios y paleogeograf\u00eda de la cuenca, que responden a episodios importantes en la estructuraci\u00f3n de la cadena pirenaica, tales como el emplazamiento de l\u00e1minas de z\u00f3calo. En las megasecuencias con dep\u00f3sitos marinos, el factor tect\u00f3nico no hace m\u00e1s que acentuar las tendencias en las facies provocadas por la curva eust\u00e1tica global, con lo que de manera especial en ellas, se registran excepcionalmente los dos factores aloc\u00edclicos principales (tect\u00f3nica y eustatismo). En las megasecuencias con sedimentos unicamente continentales, es el factor tect\u00f3nico el que condiciona su dep\u00f3sito.  el emplazamiento de l\u00e1minas de z\u00f3calo, adem\u00e1s, ser\u00eda el origen de la simultaneidad en las etapas de aceleraci\u00f3n y descaceleraci\u00f3n de una serie de estructuras individuales de evoluci\u00f3n sincr\u00f3nica con el dep\u00f3sito, que se encuentran al n y s del sinclinorio.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Estratigrafia del eoceno-oligoceno de la cuenca de jaca (sinclinorio de guarga)<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Estratigrafia del eoceno-oligoceno de la cuenca de jaca (sinclinorio de guarga) <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Montes Santiago Manuel Jes\u00fas <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Barcelona<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 20\/12\/2002<\/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>Ferran Colombo Pi\u00f1ol<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: oriol Riba arderiu <\/li>\n<li>roberto Rodr\u00edguez fern\u00e1ndez (vocal)<\/li>\n<li>cai Puigdefabregas tomas (vocal)<\/li>\n<li>eduardo Remacha grau (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Montes Santiago Manuel Jes\u00fas El sinclinorio del guarga forma parte de la cuenca sinorog\u00e9nica de jaca, situada [&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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