{"id":139503,"date":"2026-01-12T17:46:16","date_gmt":"2026-01-12T17:46:16","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/estratigrafia-y-sedimentologia-de-la-sucesion-westgaliense-del-borde-sureste-de-la-cuenca-carbonifera-central\/"},"modified":"2026-01-12T17:46:16","modified_gmt":"2026-01-12T17:46:16","slug":"estratigrafia-y-sedimentologia-de-la-sucesion-westgaliense-del-borde-sureste-de-la-cuenca-carbonifera-central","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/estratigrafia-y-sedimentologia-de-la-sucesion-westgaliense-del-borde-sureste-de-la-cuenca-carbonifera-central\/","title":{"rendered":"\u00abestratigrafia y sedimentolog\u00eda de la sucesion westgaliense del borde sureste de la cuenca carbonifera central\u00bb."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Pedro Barba Regidor <\/strong><\/h2>\n<p>La sucesion carbonifera de la zona cantabrica presenta grandes variaciones tanto laterales como verticales de facies. En el area estudiada por el sr. Barba, correspondiente a los sectores del borde sur de la cuenca carbonifera central (aller-nalon, piedrafita-lillo, lois-ciguera y porma) y al sector de san isidro de la unidad del ponga, se describen e interpretan un total de 28 facies y asociaciones de facies que han permitido al autor caracterizar diversos medios sedimentarios y proponer un modelo general para la cuenca. Del estudio de las secuencias presentes en estas sucesiones, se observa una organizacion ciclica de diverso rango constituyendo macrosecuencias, mesosecuencias y secuencias elementales o ciclotemas, proponiendose para su origen la concatenacion de procesos tectonicos y eustaticos.  arealmente, se expone la evolucion paleogeografica del carbonifero de la zona cantabrica, especialmente en lo que concierne al area de estudio; el modelo evolutivo propuesto es parcialmente equivalente al definido por tankard (1986) en los apalaches.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>\u00abestratigrafia y sedimentolog\u00eda de la sucesion westgaliense del borde sureste de la cuenca carbonifera central\u00bb.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 \u00abestratigrafia y sedimentolog\u00eda de la sucesion westgaliense del borde sureste de la cuenca carbonifera central\u00bb. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Pedro Barba Regidor <\/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>Juan  Ramon Colmenero Navarro<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Inmaculada Corrales Zarauza <\/li>\n<li>Isabel Su\u00e1rez Ruiz (vocal)<\/li>\n<li>Jes\u00fas Carballeira Cueto (vocal)<\/li>\n<li>Emilio Elizaga Mu\u00f1oz (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Pedro Barba Regidor La sucesion carbonifera de la zona cantabrica presenta grandes variaciones tanto laterales como verticales [&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 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