{"id":142313,"date":"2026-04-02T13:17:16","date_gmt":"2026-04-02T13:17:16","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/procesos-de-meteorizacion-de-rocas-graniticas-de-galicia-bajo-diferentes-ambientes-edafoclimaticos\/"},"modified":"2026-04-02T13:17:16","modified_gmt":"2026-04-02T13:17:16","slug":"procesos-de-meteorizacion-de-rocas-graniticas-de-galicia-bajo-diferentes-ambientes-edafoclimaticos","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/procesos-de-meteorizacion-de-rocas-graniticas-de-galicia-bajo-diferentes-ambientes-edafoclimaticos\/","title":{"rendered":"Procesos de meteorizacion de rocas graniticas de galicia bajo diferentes ambientes edafoclimaticos"},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Taboada Rodriguez Teresa M. <\/strong><\/h2>\n<p>Se estudian los procesos de meteorizacion de las rocas graniticas de galicia analizando trece perfiles desarrollados sobre distintos tipos de granitos (calcoalcalinos o alcalinos) tanto situados en afloramientos graniticos costeros como en zonas interiores de monta\u00f1a. En todos los casos se estudia la evolucion microestructural (analisis comparativo de laminas delgadas), mineralogica (observacion al microscopio petrografico, d.R.X. Y a.T.D.), Y geoquimica (analisis total y ph de abrasion).  globalmente se observa un proceso de meteorizacion propio de sistemas abiertos, sustractivo, con tendencia al \u00absistema residual\u00bb. El estudio de la fraccion mas evolucionada indica que se trata de un proceso fundamentalmente monosialitico, aunque en algunos de los perfiles predomine la alitizacion, especialmente en las primeras fases de meteorizacion. Excepcionalmente se observa una ligera bisialitizacion en los horizontes c de dos de los perfiles analizados, aunque en las zonas mas superficiales de estos perfiles la tendencia es monosialitica.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Procesos de meteorizacion de rocas graniticas de galicia bajo diferentes ambientes edafoclimaticos<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Procesos de meteorizacion de rocas graniticas de galicia bajo diferentes ambientes edafoclimaticos <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Taboada Rodriguez Teresa M. <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Santiago de compostela<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1993<\/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>Carlota Garcia Paz<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Felipe Mac\u00edas V\u00e1zquez <\/li>\n<li>Juan  Ram\u00f3n Vidal Roman\u00ed (vocal)<\/li>\n<li>Ward Chesworth (vocal)<\/li>\n<li>Eloy Molina Ballesteros (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Taboada Rodriguez Teresa M. Se estudian los procesos de meteorizacion de las rocas graniticas de galicia analizando [&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":[27,2498,3831,54724,3977,977],"tags":[43567,90154,3120,16164,257021,61933],"class_list":["post-142313","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-tierra-y-del-espacio","category-edafologia","category-geoquimica","category-geoquimica-de-bajas-temperaturas","category-mineralogia-de-suelos","category-santiago-de-compostela","tag-carlota-garcia-paz","tag-eloy-molina-ballesteros","tag-felipe-macias-vazquez","tag-juan-ramon-vidal-romani","tag-taboada-rodriguez-teresa-m","tag-ward-chesworth"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/142313","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=142313"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/142313\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=142313"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=142313"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=142313"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}