{"id":38651,"date":"2018-03-09T09:38:19","date_gmt":"2018-03-09T09:38:19","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/evolucion-geomorfologica-y-dinamica-de-las-vertientes-en-el-noreste-de-galicia-importancia-de-los-procesos-de-origen-frio-en-un-sector-de-las-montanas-lucenses\/"},"modified":"2018-03-09T09:38:19","modified_gmt":"2018-03-09T09:38:19","slug":"evolucion-geomorfologica-y-dinamica-de-las-vertientes-en-el-noreste-de-galicia-importancia-de-los-procesos-de-origen-frio-en-un-sector-de-las-montanas-lucenses","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/evolucion-geomorfologica-y-dinamica-de-las-vertientes-en-el-noreste-de-galicia-importancia-de-los-procesos-de-origen-frio-en-un-sector-de-las-montanas-lucenses\/","title":{"rendered":"Evolucion geomorfologica y dinamica de las vertientes en el noreste de galicia. importancia de los procesos de origen frio en un sector de las monta\u00f1as lucenses."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Marcos Valc\u00e1rcel D\u00edaz <\/strong><\/h2>\n<p>La presente memoria tiene como objetivo la reconstrucci\u00f3n de la din\u00e1mica geomorfol\u00f3gica y de las condiciones paleoambientales durante los momentos fr\u00edos del cuaternario reciente en las sierras nordorientales de lugo- xistral, meira, montes de a fonsagrada, oiribio, montes de o cebreiro y serra dos ancares,esta \u00faltima tambi\u00e9n en territorio leon\u00e9s- cuyas altitudes oscilan entre los 1000 y 2000 metros.  en el primer cap\u00edtulo se definen los objetivos, el \u00e1rea de estudio y la metodolog\u00eda a utilizar. Esta ha sido la usual en la investigaci\u00f3n geomorfol\u00f3gica, incluyendo trabajo de campo, de laboratorio y de gabinete. Un segundo capitulo de la memoria se ha dedicado a la revisi\u00f3n de los antecedentes sobre la evoluci\u00f3n de las formas del relieve en galicia, con especial atenci\u00f3n a su sector nordoriental, mientras que en el tercero se realiza una revisi\u00f3n de las aportaciones de anteriores investigadores sobre el \u00e1rea de estudio. Tras un amplio cap\u00edtulo dedicado a la revision conceptual de los t\u00e9rminos existentes en la literatura cientifica al uso, se aborda la descripci\u00f3n y el an\u00e1lisis detallado de las formas y de los dep\u00f3sitos de origen glaciar y periglaciar. Posteriormente se establece una sintesis general, se relacionan los procesos y su cronolog\u00eda, tanto relativa como absoluta, y se aborda la reconstrucci\u00f3n paleoambiental a partir del establecimiento de diferentes modelos geocriol\u00f3gicos.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Evolucion geomorfologica y dinamica de las vertientes en el noreste de galicia. importancia de los procesos de origen frio en un sector de las monta\u00f1as lucenses.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Evolucion geomorfologica y dinamica de las vertientes en el noreste de galicia. importancia de los procesos de origen frio en un sector de las monta\u00f1as lucenses. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Marcos Valc\u00e1rcel D\u00edaz <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Santiago de compostela<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 29\/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>Augusto P\u00e9rez Albert\u00ed<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Jos\u00e9 manuel Rubio recio <\/li>\n<li>Antonio Gomez ortiz (vocal)<\/li>\n<li>Antonio Mart\u00ednez cortizas (vocal)<\/li>\n<li>Jos\u00e9 Luis Pe\u00f1a monne (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Marcos Valc\u00e1rcel D\u00edaz La presente memoria tiene como objetivo la reconstrucci\u00f3n de la din\u00e1mica geomorfol\u00f3gica y de [&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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