{"id":118724,"date":"2022-07-17T04:55:01","date_gmt":"2022-07-17T04:55:01","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/sand-tongues-de-la-unidad-de-broto-grupo-de-hecho-entre-el-anticlinal-de-boltana-y-el-rio-osia-prov-de-huesca\/"},"modified":"2022-07-17T04:55:01","modified_gmt":"2022-07-17T04:55:01","slug":"sand-tongues-de-la-unidad-de-broto-grupo-de-hecho-entre-el-anticlinal-de-boltana-y-el-rio-osia-prov-de-huesca","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/sand-tongues-de-la-unidad-de-broto-grupo-de-hecho-entre-el-anticlinal-de-boltana-y-el-rio-osia-prov-de-huesca\/","title":{"rendered":"\u00absand tongues\u00bb de la unidad de broto (grupo de hecho), entre el anticlinal de bolta\u00f1a y el rio osia (prov. de huesca)."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Eduardo Remacha Grau <\/strong><\/h2>\n<p>Propuesta de metodolog\u00eda de campo en sedimentos tursiditicos. Estudio de los ciclos de compensacion como producto de procesos de acrecion vertical. Estos ciclos son las autenticas unidades secuenciales de los depositos del sistema de acumulacion.  analisis y significado sedimentologico de algunas de las capas que forman estos ciclos de compensacion. Estudio de los ciclos de facies en funcion de la velocidad de sedimentacion y cantidad de deformacion tectomica. Se descarta la posibilidad de que estos sedimentos se hayan visto sometidos a progradacion. Se ha calculado que la continuidad lateral de las capas  en corte paralelo a las paleocorrientes  es de mas de 110 km  y la anchura de estos cuerpos aselmolsos  en corte normal a las pateocorrientes es de 10 km  por ello se descartan los terminos  cosulo  y  abanico .<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>\u00absand tongues\u00bb de la unidad de broto (grupo de hecho), entre el anticlinal de bolta\u00f1a y el rio osia (prov. de huesca).<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 \u00absand tongues\u00bb de la unidad de broto (grupo de hecho), entre el anticlinal de bolta\u00f1a y el rio osia (prov. de huesca). <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Eduardo Remacha Grau <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Aut\u00f3noma de barcelona<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1984<\/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 Rosell Sanuy<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Emiliano Mutti <\/li>\n<li>Lorenzo Vilas Minondo (vocal)<\/li>\n<li>Alberto Garrido Mejias (vocal)<\/li>\n<li>Antonio Obrador Tuduri (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Eduardo Remacha Grau Propuesta de metodolog\u00eda de campo en sedimentos tursiditicos. Estudio de los ciclos de compensacion [&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":[27,245,953,3857],"tags":[232888,19690,63557,115739,473,5043],"class_list":["post-118724","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-tierra-y-del-espacio","category-estratigrafia","category-geologia","category-sedimentologia","tag-alberto-garrido-mejias","tag-antonio-obrador-tuduri","tag-eduardo-remacha-grau","tag-emiliano-mutti","tag-juan-rosell-sanuy","tag-lorenzo-vilas-minondo"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/118724","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=118724"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/118724\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=118724"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=118724"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=118724"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}