{"id":12700,"date":"2018-03-09T08:58:40","date_gmt":"2018-03-09T08:58:40","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/tectonica-cenozoica-en-el-dominio-cortical-de-alboran\/"},"modified":"2018-03-09T08:58:40","modified_gmt":"2018-03-09T08:58:40","slug":"tectonica-cenozoica-en-el-dominio-cortical-de-alboran","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/tectonica-cenozoica-en-el-dominio-cortical-de-alboran\/","title":{"rendered":"Tectonica cenozoica en el dominio cortical de alboran"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Guillermo Booth Rea <\/strong><\/h2>\n<p>La tesis doctoral propone un modelo de evolucion tectonica del dominio cortical de alboran (dca), aflorante en la rama norte del arco de gibraltar, durante el cenozoico, haciendo especial enfasis en la geometria, cinematica y cronolog\u00eda de las estructuras formadas en ese periodo de tiempo y difereciando los episodios tectonicos mas relevantes. Para esto se han seleccionado, para su estudio, tres areas emergidas representativas de distintas posiciones estructurales del dominio cortical de alboran, poco estudiadas previamente, y con una cobertera sedimentaria que permitiese establecer  la relaci\u00f3n tectonica entre las estructuras que afectan al dca y la geometria del relleno sedimentario. Ademas se ha determinado la estructura, mediante el procesado e interpretacion de los perfiles sismicos de reflexion profunda esci alb 2b y 2c, de un area sumergida, representativa de la transicion entre corteza continental adelgazada, constituida por rocas del dca y volcanicas, y corteza oceanica de las cuencas de alboran y surbalear respectivamente.  las areas emergidas seleccionadas han sido las siguientes:  un sector de las beticas occidentales, situado al w del meridiano de malaga y que incluye la cuenca de la hoya de malaga y las sierras de la axarquia occidental, constituidas por rocas del dominio cortical de alboran. en este area se han diferenciado dos sistemas extensionales con transporte tect\u00f3nico hacia el ssw y nnw responsables del adelgazamiento del dominio cortical de alboran hasta constituir el basamento de la hoya de malaga, especialmente subsidente durante el mioceno inferior.  se ha seleccionado un area representativa de las b\u00e9ticas nororientales que incluye a la cuenca de lorca y los relieves que la circundan, correspondientes a las sierras de las estancias, de la tercia y de espu\u00f1a. En este sector se ha estudiado la evolucion tectonometamorfica de unidades del dominio cortical de alboran, asi como las estructuras fragiles que consti<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Tectonica cenozoica en el dominio cortical de alboran<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Tectonica cenozoica en el dominio cortical de alboran <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Guillermo Booth Rea <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Granada<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 13\/09\/2001<\/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>Victor Garcia Due\u00f1as<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal:  Comas minondo Mar\u00eda  del carmen <\/li>\n<li>Francisco Navarro vila (vocal)<\/li>\n<li>Andr\u00e9s Perez estaun (vocal)<\/li>\n<li>Jos\u00e9 Miguel Aza\u00f1on hernandez (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Guillermo Booth Rea La tesis doctoral propone un modelo de evolucion tectonica del dominio cortical de alboran [&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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