{"id":36046,"date":"1998-01-01T00:00:00","date_gmt":"1998-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/caracterizacion-petrologica-y-geoquimica-del-sector-oriental-del-batolito-de-los-pedroches\/"},"modified":"1998-01-01T00:00:00","modified_gmt":"1998-01-01T00:00:00","slug":"caracterizacion-petrologica-y-geoquimica-del-sector-oriental-del-batolito-de-los-pedroches","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/caracterizacion-petrologica-y-geoquimica-del-sector-oriental-del-batolito-de-los-pedroches\/","title":{"rendered":"Caracterizacion petrologica y geoquimica del sector oriental del batolito de los pedroches."},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Larrea Bilbao Francisco Jose <\/strong><\/h2>\n<p>El batolito de los pedroches, situado en la parte meridional de la zona centroib\u00e9rica, constituye una importante alineaci\u00f3n magm\u00e1tica tardiherc\u00ednica, emplazada en ambiente geodin\u00e1mico transtensional. Est\u00e1 formado por dos unidades plut\u00f3nicas: granodior\u00edtica y gran\u00edtica.  ambas unidades est\u00e1n atravesadas por numerosos diques \u00e1cidos. La secuencia temporal de emplazamiento es la siguiente: granodioritas, adamellitas biot\u00edticas s.L., granitos biot\u00edticos porf\u00eddicos s.L., Leucogranitos y complejo filoniano en el que destacan los diques de la red no-se.  petrogr\u00e1ficamente se constata escasa variaci\u00f3n mineral\u00f3gica entre los litotipos principales, son rocas con mineralog\u00eda gran\u00edtica banal, con espor\u00e1dica cordierita, moscovita secundaria y apatito, circ\u00f3n e ilmenita como accesorios. En los diagramas qap ocupan mayoritariamente el campo de las rocas de origen crustal (lameyre y bowden, 1982), definiendo pautas evolutivas de series calcoalcalinas granodior\u00edticas o medias en potasio.  las tendencias de variaci\u00f3n qu\u00edmica denotan un descenso en al\u00famina, ferromagnesianos y cal, y enriquecimiento en \u00e1lcalis con el incremento en sio2. Unido a las pautas segmentadas observadas en algunos elementos traza caracteristicos en procesos de cristalizaci\u00f3n fraccionada. Estas tendencias se explican por la fraccionaci\u00f3n de plagioclasa, biotita, feldespato pot\u00e1sico, +- accesorios. Las litolog\u00edas mayoritarias corresponden a los t\u00e9rminos peraluminosos de una asociaci\u00f3n alum\u00ednico caf\u00e9mica calcoalcalina (debon &amp; le fort, 1983) o calcoalcalina alta en potasio (peccerillo &amp; taylor, 1976).  los datos isot\u00f3picos disponibles advierten de la posible participaci\u00f3n de materiales corticales y mant\u00e9licos en el origen del batolito de los pedroches, lo cual resulta sugerente como hip\u00f3tesis petrogen\u00e9tica.  el plut\u00f3n de santa elena representa la zona apical de otra importante manifestaci\u00f3n \u00edgnea tardiherc\u00ednica m\u00e1s septen<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Caracterizacion petrologica y geoquimica del sector oriental del batolito de los pedroches.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Caracterizacion petrologica y geoquimica del sector oriental del batolito de los pedroches. <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Larrea Bilbao Francisco Jose <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Pa\u00eds vasco\/euskal herriko unibertsitatea<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/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>Juan  Ignacio Gil Ibarguchi<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Luis Guillermo Corretg\u00e9 Casta\u00f1\u00f3n <\/li>\n<li>Felix Bellido Mulas (vocal)<\/li>\n<li> Tubia Martinez Jos\u00e9 M. (vocal)<\/li>\n<li>Antonio Castro Dorado (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Larrea Bilbao Francisco Jose El batolito de los pedroches, situado en la parte meridional de la zona [&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":[27,16139,953,3831,12909,3436],"tags":[4380,65710,9064,95730,5133,57787],"class_list":["post-36046","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-tierra-y-del-espacio","category-distribucion-de-oligoelementos","category-geologia","category-geoquimica","category-pais-vasco-euskal-herriko-unibertsitatea","category-petrologia-ignea-y-metamorfica","tag-antonio-castro-dorado","tag-felix-bellido-mulas","tag-juan-ignacio-gil-ibarguchi","tag-larrea-bilbao-francisco-jose","tag-luis-guillermo-corretge-castanon","tag-tubia-Martinez-jose-m"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/36046","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=36046"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/36046\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=36046"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=36046"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=36046"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}