{"id":85127,"date":"2018-03-10T00:09:33","date_gmt":"2018-03-10T00:09:33","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/el-relieve-de-los-montes-obarenesburgos\/"},"modified":"2018-03-10T00:09:33","modified_gmt":"2018-03-10T00:09:33","slug":"el-relieve-de-los-montes-obarenesburgos","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/el-relieve-de-los-montes-obarenesburgos\/","title":{"rendered":"El relieve de los montes obarenes(burgos)"},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Morales Rodriguez Cargos Gabriel <\/strong><\/h2>\n<p>Se plantea el estudio del relieve de un \u00e1rea de monta\u00f1a media, los montes obarenes, limite meridional de las monta\u00f1as de burgos en el contacto con la bureba. Se trata de confirmar el car\u00e1cter estructural del relieve y la importancia que adquiere en su construccion la acci\u00f3n de la tect\u00f3nica intrusiva en este tipo de bordes as\u00ed como la incidencia de la morfotect\u00f3nica en una zona que est\u00e1 afectada por una red hidrogr\u00e1fica antigua, de comportamiento complejo, tanto epig\u00e9nico como antecedente, adaptada e inadaptada. Asimismo se pretende verificar la unidad morfoestructural de este umbral monta\u00f1oso.  para ello se ha realizado una interpretaci\u00f3n detallada del relieve a partir del an\u00e1lisis de las morfoestructuras que integran los montes obarenes y se elabora la cartograf\u00eda morfoestrucutral, que se ha sintetizado en diez esquemas morfoestructurales y setenta y cinco cortes geomorfol\u00f3gicos as\u00ed como bloques diagrama de car\u00e1cter evolutivo.  el trabajo ha permitido verificar las hipotesis de partida y se\u00f1alar como el relieve de los montes obarenes es un relieve estructural conformado como un haz de pliegues que con direccion ono-ese se suceden en relevo paralelos al borde tect\u00f3nico burebano,como expresi\u00f3n de las deformaciones propias de una cadena de pliegues de cobertera, a partir de la acci\u00f3n de una tect\u00f3nica intrusiva tard\u00eda que ha deformado los relieves anteriores y en los que ha sido protagonista la presencia de una superficie de erosi\u00f3n pol\u00edg\u00e9nica.Asimismo se constata la subordinaci\u00f3n de los procesos erosivos a los factores litol\u00f3gicos y tect\u00f3nicos en la construcci\u00f3n del relieve.  se define as\u00ed un plegamiento caracteristico de borde de depresi\u00f3n tect\u00f3nica, a escala local, de haces de pliegues en relevo paralelos al borde tect\u00f3nico,donde las deformaciones son polig\u00e9nicos y hay episodios de una tect\u00f3nica de fractura asociada a procesos intrusivos de car\u00e1cter diap\u00edrico. Tambi\u00e9n se se\u00f1ala la coexistencia de<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>El relieve de los montes obarenes(burgos)<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 El relieve de los montes obarenes(burgos) <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Morales Rodriguez Cargos Gabriel <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Valladolid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 19\/06\/2000<\/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>Jes\u00fas Garcia Fernandez<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: enrique Matarredona coll <\/li>\n<li>Juan  Antonio Marco molina (vocal)<\/li>\n<li>julio Mu\u00f1oz jimenez (vocal)<\/li>\n<li> Poblete piedrabuena Miguel angel (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Morales Rodriguez Cargos Gabriel Se plantea el estudio del relieve de un \u00e1rea de monta\u00f1a media, los [&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 center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"ast-content-background-meta":{"desktop":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"footnotes":""},"categories":[27,5742,5741,953,75,12451],"tags":[19357,95501,79861,24591,179425,179426],"class_list":["post-85127","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-tierra-y-del-espacio","category-ciencias-geograficas","category-geografia-fisica","category-geologia","category-geomorfologia","category-valladolid","tag-enrique-matarredona-coll","tag-jesus-garcia-fernandez","tag-juan-antonio-marco-molina","tag-julio-munoz-jimenez","tag-morales-rodriguez-cargos-gabriel","tag-poblete-piedrabuena-miguel-angel"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/85127","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/comments?post=85127"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/85127\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=85127"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=85127"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=85127"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}