{"id":46145,"date":"2019-09-16T23:40:49","date_gmt":"2019-09-16T23:40:49","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/interpretacion-de-detalle-del-ambiente-de-sedimentacion-de-la-formacion-productiva-del-yacimiento-petrolifero-de-ayoluengo\/"},"modified":"2019-09-16T23:40:49","modified_gmt":"2019-09-16T23:40:49","slug":"interpretacion-de-detalle-del-ambiente-de-sedimentacion-de-la-formacion-productiva-del-yacimiento-petrolifero-de-ayoluengo","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/interpretacion-de-detalle-del-ambiente-de-sedimentacion-de-la-formacion-productiva-del-yacimiento-petrolifero-de-ayoluengo\/","title":{"rendered":"Interpretacion de detalle del ambiente de sedimentacion de la formacion productiva del yacimiento petrolifero de ayoluengo"},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Garcia Si\u00f1eriz Butrague\u00f1o Bonifacio <\/strong><\/h2>\n<p>Haciendo uso de la curva de potencial espontaneo obtenida en sondeos de ayoluengo y otros criterios (geomorfologicos  litologicos  etc)  se llega a determinar el ambiente deposicional  cuya tesis es que se trata de una llanura aluvio deltaica durante el purbeckiense  asi como se concluye en que la generacion de petroleo tuvo lugar durante el valanginiense en rocas madre clasicas  redistribuyendose el petroleo durante el terciario. Finalmente  se esbozan objetivos remanentes para una investigacion mas profunda.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Interpretacion de detalle del ambiente de sedimentacion de la formacion productiva del yacimiento petrolifero de ayoluengo<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Interpretacion de detalle del ambiente de sedimentacion de la formacion productiva del yacimiento petrolifero de ayoluengo <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Garcia Si\u00f1eriz Butrague\u00f1o Bonifacio <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Polit\u00e9cnica de Madrid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1979<\/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> Rios Garcia Jos\u00e9 M.<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Tirso Febrel Molinero <\/li>\n<li>Indalecio Quintero Amador (vocal)<\/li>\n<li> Rios Garcia Jos\u00e9 M. (vocal)<\/li>\n<li>Manuel Lopez Linares (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Garcia Si\u00f1eriz Butrague\u00f1o Bonifacio Haciendo uso de la curva de potencial espontaneo obtenida en sondeos de ayoluengo [&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":[27,953,5040,16008],"tags":[110836,71175,108610,109734,108605],"class_list":["post-46145","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-tierra-y-del-espacio","category-geologia","category-geologia-del-petroleo","category-politecnica-de-madrid","tag-garcia-sineriz-butragueno-bonifacio","tag-indalecio-quintero-amador","tag-manuel-lopez-linares","tag-rios-garcia-jose-m","tag-tirso-febrel-molinero"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/46145","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=46145"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/46145\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=46145"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=46145"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=46145"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}