{"id":139538,"date":"2026-01-12T17:46:30","date_gmt":"2026-01-12T17:46:30","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/relaciones-entre-la-petrologia-y-la-geoquimica-de-la-materia-organica-en-pizarras-bituminosas-espanolas\/"},"modified":"2026-01-12T17:46:30","modified_gmt":"2026-01-12T17:46:30","slug":"relaciones-entre-la-petrologia-y-la-geoquimica-de-la-materia-organica-en-pizarras-bituminosas-espanolas","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/relaciones-entre-la-petrologia-y-la-geoquimica-de-la-materia-organica-en-pizarras-bituminosas-espanolas\/","title":{"rendered":"\u00abrelaciones entre la petrolog\u00eda y la geoquimica de la materia organica en pizarras bituminosas espa\u00f1olas.\u00bb"},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Gomez Borrego M. Angeles <\/strong><\/h2>\n<p>En este trabajo se estudia la materia organica de las pizarras bituminosas de cuatro localidades espa\u00f1olas diferentes en edad y origen: puertollano (estefaniense), rubielos de mora (mioceno), llames de parres-asturias (cretacico) y fm. Armancies (eoceno marino catalan). El estudio se aborda utilizando diferentes tecnicas instrumentales de caracter petrografico (microscopia optica y de barrido) y geoquimico (analisis elemental, pirolisis rockeval, termogravimetria, cromatografia de gases\/ espectrometria de masas, espectroscopia de infrarrojos y resonancia magnetica nuclear). Se pretende estudiar en profundidad la riqueza tipo de materia organica y grado de evolucion de las pizarras, y comprobar el grado de congruencia entre los resultados obtenidos por las diferentes tecnicas.  se confirma un origen lacustre para las pizarras de puertollano, llames y rubielos de mora (tipo i) y marino para las de la fm. Armancies (tipo ii). El grado de evolucion determinado a partir de diferentes parametros indica que la materia organica de rubielos de mora es extremadamente inmadura, inmadura la de llames de parres e inmadura pero proxima al transito diagenesis\/catagenesis la de puertollano, mientras que las muestras de la fm.  armancies estan al inicio de la formacion de aceites. Se establece un aumento de la evolucion dentro de la serie de puertollano y de la fm. Armancies. Destaca el alto grado de congruencia de los resultados obtenidos por las diferentes tecnicas analiticas.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>\u00abrelaciones entre la petrolog\u00eda y la geoquimica de la materia organica en pizarras bituminosas espa\u00f1olas.\u00bb<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 \u00abrelaciones entre la petrolog\u00eda y la geoquimica de la materia organica en pizarras bituminosas espa\u00f1olas.\u00bb <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Gomez Borrego M. Angeles <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Oviedo<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1992<\/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>Jose Gutierrez Blanco<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Sousa Lemos De <\/li>\n<li>Pablo Luis Bernad Enguita (vocal)<\/li>\n<li>Carmen Dorronsoro Urrutia (vocal)<\/li>\n<li>Juan  Ramon Colmenero Navarro (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Gomez Borrego M. Angeles En este trabajo se estudia la materia organica de las pizarras bituminosas de [&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":[27,245,953,8846,25320],"tags":[20456,83827,254049,5044,50309,254050],"class_list":["post-139538","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-tierra-y-del-espacio","category-estratigrafia","category-geologia","category-oviedo","category-petrologia-sedimentaria","tag-carmen-dorronsoro-urrutia","tag-gomez-borrego-m-angeles","tag-jose-gutierrez-blanco","tag-juan-ramon-colmenero-navarro","tag-pablo-luis-bernad-enguita","tag-sousa-lemos-de"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/139538","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=139538"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/139538\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=139538"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=139538"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=139538"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}