{"id":34753,"date":"1998-01-01T00:00:00","date_gmt":"1998-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/geomorfologia-de-un-sector-comprendido-entre-las-provincias-de-lugo-y-ourense-galicia\/"},"modified":"1998-01-01T00:00:00","modified_gmt":"1998-01-01T00:00:00","slug":"geomorfologia-de-un-sector-comprendido-entre-las-provincias-de-lugo-y-ourense-galicia","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/geomorfologia-de-un-sector-comprendido-entre-las-provincias-de-lugo-y-ourense-galicia\/","title":{"rendered":"Geomorfolog\u00eda de un sector comprendido entre las provincias de lugo y ourense. galicia."},"content":{"rendered":"

Tesis doctoral de Jorge Yepes Temi\u00f1o <\/strong><\/h2>\n

El \u00e1rea estudiada queda delimitada por la hoja del m.T.N. n 17-27 (e: 1\/200.000): y se encuentra en el se de galicia. Seg\u00fan julivert (1972) queda encuadrada en la zona centro ib\u00e9rica del macizo hesp\u00e9rico peninsular. En este trabajo se revisan algunos criterios geomorfol\u00f3gicos para esclarecer las relaciones relieve-tectonica alpina. 1. Se realiz\u00f3 una cartografia geomorfol\u00f3gica regional (e: 1\/100.000 y 1\/50.000): reconoci\u00e9ndose ocho replanos, en general bastante degradados (r1600, r1400, r1200, r1000, r800, r600, r500 y r100). Su an\u00e1lisis revel\u00f3: 1) una distribuci\u00f3n an\u00f3mala y desigual de sus extensiones: 2)un origen por corrosi\u00f3n quimica en tres casos (r1600, r800 y r400) y por erosi\u00f3n fluvial en el resto; 3)una relaci\u00f3n entre la mayor\u00eda de las fosas cartografiadas y dos de los replanos (r600 y r400); 4)una diferenciaci\u00f3n morfol\u00f3gica de las superficies (superficies rampa y superficies huecas) atribuible a diferentes estadios del desmantelamiento de los replanos; 5)la existencia de terrazas erosivas dentro de cada replano, lo que permiti\u00f3 identificar redes f\u00f3siles parcialmente capturadas; y 6)la importancia morfoestructural de las direcciones nnw-sse a nw-se y ene- wsw a en-sw. De forma provisional se ha propuesto una secuencia de eventos, entre los que destacan dos pulsos tect\u00f3nicos. El primero habr\u00eda afectado a las fracturas en-sw y se le atribuir\u00eda el descabalamiento de la r800. El segundo pulso habr\u00eda afectado a las fracturas nnw-sse y propiciando la fosilizaci\u00f3n parcial de la depresi\u00f3n de xinzo de limia por la de maceda. 2. Se analiz\u00f3 la geometr\u00eda de la red fluvial: observ\u00e1ndose dos trazados, uno centr\u00edpeto y otro en bayoneta. El trazado centr\u00edpeto se observ\u00f3 asociado a superficies con morfolog\u00eda hueca y el trazado en bayoneta a superficies tipo rampa. Adem\u00e1s se caracterizaron cinco tipos de cursos fluviales: 1) valles muy evolucionados (muy encajados, con meandros epig\u00e9nicos, pendient<\/p>\n

 <\/p>\n

Datos acad\u00e9micos de la tesis doctoral \u00abGeomorfolog\u00eda de un sector comprendido entre las provincias de lugo y ourense. galicia.<\/strong>\u00ab<\/h3>\n
    \n
  • T\u00edtulo de la tesis:<\/strong>\u00a0 Geomorfolog\u00eda de un sector comprendido entre las provincias de lugo y ourense. galicia. <\/li>\n
  • Autor:<\/strong>\u00a0 Jorge Yepes Temi\u00f1o <\/li>\n
  • Universidad:<\/strong>\u00a0 Complutense de Madrid<\/li>\n
  • Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1998<\/li>\n<\/ul>\n

     <\/p>\n

    Direcci\u00f3n y tribunal<\/h3>\n
      \n
    • Director de la tesis<\/strong>\n
        \n
      • Juan Ram\u00f3n Vidal Roman\u00ed<\/li>\n<\/ul>\n<\/li>\n
      • Tribunal<\/strong>\n
          \n
        • Presidente del tribunal: Pedraza Gilsanz JavierDe <\/li>\n
        • Angel Martin Serrano (vocal)<\/li>\n
        • Joan Manuel Vilaplana Fernandez (vocal)<\/li>\n
        • U\u00f1a Alvarez Elena De (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n

           <\/p>\n","protected":false},"excerpt":{"rendered":"

          Tesis doctoral de Jorge Yepes Temi\u00f1o El \u00e1rea estudiada queda delimitada por la hoja del m.T.N. n 17-27 (e: 1\/200.000): […]<\/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":[27,953,75],"tags":[60664,41663,93455,16164,38972,93456],"class_list":["post-34753","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-tierra-y-del-espacio","category-geologia","category-geomorfologia","tag-angel-martin-serrano","tag-joan-manuel-vilaplana-fernandez","tag-jorge-yepes-temino","tag-juan-ramon-vidal-romani","tag-pedraza-gilsanz-javierde","tag-una-alvarez-elena-de"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/34753","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=34753"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/34753\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=34753"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=34753"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=34753"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}