{"id":85484,"date":"2018-03-10T00:09:57","date_gmt":"2018-03-10T00:09:57","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/las-rocas-plutonicas-calcoalcalinas-y-shoshoniticas-del-domo-varisco-del-tormescentro-oeste-espanol-estudio-mineralogico-geoqua%c2%admico-y-petrogenico\/"},"modified":"2018-03-10T00:09:57","modified_gmt":"2018-03-10T00:09:57","slug":"las-rocas-plutonicas-calcoalcalinas-y-shoshoniticas-del-domo-varisco-del-tormescentro-oeste-espanol-estudio-mineralogico-geoqua%c2%admico-y-petrogenico","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/las-rocas-plutonicas-calcoalcalinas-y-shoshoniticas-del-domo-varisco-del-tormescentro-oeste-espanol-estudio-mineralogico-geoqua%c2%admico-y-petrogenico\/","title":{"rendered":"Las rocas plutonicas calcoalcalinas y shoshoniticas del domo varisco del tormes(centro-oeste espa\u00f1ol). estudio mineral\u00f3gico, geoqu\u00edmico y petrogenico."},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Lopez Moro Francisco Javier <\/strong><\/h2>\n<p>En el domo varisco del tormes se han diferenciado tres asociaciones de rocas en funci\u00f3n de sus diferentes contenidos en feldespato pot\u00e1sico, k,p y lree:  a)asociaci\u00f3n dior\u00edtica, con t\u00e9rminos desde dioritas a tonalitas  b)asociaci\u00f3n granodior\u00edtica, con t\u00e9rminos desde monzodioritas hasta sienogranitos y que incluye a vaugneritas.  c)asociaci\u00f3n monzon\u00edtica con un rango composicional desde monzodioritas a cuarzomonzonitas porfidico-biot\u00edticas y espor\u00e1dicamente granitos.  desde el punto de vista del quimismo, la asociaci\u00f3n dior\u00edtica es calcoalcalina de alto k, mientras que las otras dos son afines a las shoshonitas.  a partir del estudio qu\u00edmico-mineral\u00f3gico se establece la naturaleza hidratada(4-5% h2 o) y oxidante(condiciones por encima del tamp\u00f3n ni-nio) de estos magmas. Los c\u00e1lculos geotermom\u00e9tricos indican presiones de emplazamiento en torno a 3,5-4 kbar para las rocas intermedias y entre 4-5 kbar para los granitos. Las temperaturas l\u00edquidus calculadas est\u00e1n en el rango entre 1060-950\u00c2\u00bac para las rocas b\u00e1sicas e intermedias y 870-790\u00c2\u00ba c para los granitoides porfidicos.  a partir del feldespato pot\u00e1sico se pone de manifiesto una historia subs\u00f3lidus hasta 560-530 \u00c2\u00ba c seg\u00fan un solvus incoherente(con fluidos) y por debajo de 530\u00c2\u00ba c sin fluidos o seg\u00fan un solvus coherente salvo en algunos casos particulares de granitoides afectados por cizallas subverticales donde ha habido una circulaci\u00f3n de fluidos importante por debajo de los 530 \u00c2\u00bac. A trav\u00e9s de esta fase se observa un estado estructural desordenado para las rocas intermedias, cuyos feldespatos pot\u00e1sicos son ricos en componente ort\u00f3sico, y estados estructurales ordenados en granitos, de feldespatos pot\u00e1sicos m\u00e1s s\u00f3dicos.  se establece  el car\u00e1cter acumulado de los n\u00facleos corro\u00eddos de palgioclasa y la presencia de apatito heredado.  la evoluci\u00f3n para cada asociaci\u00f3n est\u00e1 relacionada con procesos afc. se constata una mayor grado de contam<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Las rocas plutonicas calcoalcalinas y shoshoniticas del domo varisco del tormes(centro-oeste espa\u00f1ol). estudio mineral\u00f3gico, geoqu\u00edmico y petrogenico.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Las rocas plutonicas calcoalcalinas y shoshoniticas del domo varisco del tormes(centro-oeste espa\u00f1ol). estudio mineral\u00f3gico, geoqu\u00edmico y petrogenico. <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Lopez Moro Francisco Javier <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Salamanca<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 30\/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>Miguel Lopez Plaza<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: mercedes Peinado moreno <\/li>\n<li>Antonio Castro dorado (vocal)<\/li>\n<li>Luis guillermo Corretg\u00e9 casta\u00f1\u00f3n (vocal)<\/li>\n<li>Francisco Martinez (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Lopez Moro Francisco Javier En el domo varisco del tormes se han diferenciado tres asociaciones de rocas [&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":[27,14353,953,3831,3931,232,3436,9386],"tags":[4380,4911,179963,5133,94274,102060],"class_list":["post-85484","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-tierra-y-del-espacio","category-geocronologia-y-radioisotopos","category-geologia","category-geoquimica","category-geoquimica-de-altas-temperaturas","category-mineralogia","category-petrologia-ignea-y-metamorfica","category-salamanca","tag-antonio-castro-dorado","tag-francisco-Martinez","tag-lopez-moro-francisco-javier","tag-luis-guillermo-corretge-castanon","tag-mercedes-peinado-moreno","tag-miguel-lopez-plaza"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/85484","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=85484"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/85484\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=85484"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=85484"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=85484"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}