{"id":50747,"date":"2021-06-07T22:17:44","date_gmt":"2021-06-07T22:17:44","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/estudi-del-glaciarisme-quaternari-de-les-altes-valls-de-la-ribagorca\/"},"modified":"2021-06-07T22:17:44","modified_gmt":"2021-06-07T22:17:44","slug":"estudi-del-glaciarisme-quaternari-de-les-altes-valls-de-la-ribagorca","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/estudi-del-glaciarisme-quaternari-de-les-altes-valls-de-la-ribagorca\/","title":{"rendered":"Estudi del glaciarisme quaternari de les altes valls de la ribagorca."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Joan Manuel Vilaplana Fernandez <\/strong><\/h2>\n<p>Aquest treball representa un estudi geomorfologic regional en el cual s ha realitzat una cartografia geomorfologica a escala 1:50.000. Es posa especial interes en l estudi cartografic  sedimentologic i estratigrafic de les principals formacions sedimentaries dledat quaternaria: acumulacions glacials (tills) glacio-lacustres  glacio-fluvials  periglacials i fluvio-torrencials. El protagoniame de l accio morfogenetica glacial  en aquest sector del pirineu central ha permes reconstruir una successio de diferents episodis glacials quaternaris  il. Lustrats amb models deposicionals concrets. Finalment s ha establert una litoestratigrafia a nivell de conca la qual ha pogut ser recolzada amb datacions absolutes i amb corelacions  amb d altres sectors del pirineu.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Estudi del glaciarisme quaternari de les altes valls de la ribagorca.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Estudi del glaciarisme quaternari de les altes valls de la ribagorca. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Joan Manuel Vilaplana Fernandez <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Barcelona<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1983<\/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>David Serrat Congost<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal:  Fontbote Mussolas Jos\u00e9 Mar\u00eda <\/li>\n<li>Oriol Riba Arderiu (vocal)<\/li>\n<li>Salvador Deguant Serra (vocal)<\/li>\n<li>Christian Schlucheer (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Joan Manuel Vilaplana Fernandez Aquest treball representa un estudi geomorfologic regional en el cual s ha realitzat [&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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