{"id":4721,"date":"1995-01-01T00:00:00","date_gmt":"1995-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/1995\/01\/01\/neotectonica-en-la-cuenca-del-bajo-segura-extremo-oriental-de-la-cordillera-betica\/"},"modified":"1995-01-01T00:00:00","modified_gmt":"1995-01-01T00:00:00","slug":"neotectonica-en-la-cuenca-del-bajo-segura-extremo-oriental-de-la-cordillera-betica","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/neotectonica-en-la-cuenca-del-bajo-segura-extremo-oriental-de-la-cordillera-betica\/","title":{"rendered":"Neotectonica en la cuenca del bajo segura (extremo oriental de la cordillera betica)."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Pedro Alfaro Garcia <\/strong><\/h2>\n<p>Se ha realizado un analisis de la evolucion geodinamica de la cuenca durante la etapa neotectonica (ultimos 11 m.A.). El relleno de la cuenca ha sido separado en cinco unidades: ms-i (tortoniense inferior), ms-ii (tortoniense superior), ms-iii (tortoniense term.-Messiniense), p (plioceno inferior) y p-q (plioceno superior-cuaternario). Los estudios de macro y microtectonica reflejan una situacion compresiva durante toda la etapa neotectonica. El campo de esfuerzos maximos en la horizontal es de direccion nnw-sse\/n-s. Del analisis estratigrafico se deducen tres eventos tectonicos principales: \u00abintratortoniense\u00bb, \u00abmessiniense basal\u00bb, e \u00abintraplioceno\u00bb. De la geofisica se deducen surcos y umbrales en el basamento controlados por los accidentes de direccion ene-wsw\/ne-sw y nw-se. Durante la etapa neotectonica la deformacion migra de n a s; en el mioceno superior actua el accidente de crevillente, y en el plioceno-cuaternario lo hace el accidente del bajo-segura. Otros accidentes activos son las fallas nw-se y el accidente los hondones. El analisis de los mecanismos focales (por el metodo de los diedros rectos) revela una situacion actual comprensiva, con una direccion de maximo esfuerzo compresivo nnw-sse.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Neotectonica en la cuenca del bajo segura (extremo oriental de la cordillera betica).<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Neotectonica en la cuenca del bajo segura (extremo oriental de la cordillera betica). <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Pedro Alfaro Garcia <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Alicante<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1995<\/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>Antonio Estevez  Rubio<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Pere Santanach Prat <\/li>\n<li>Carlos L\u00f3pez Casado (vocal)<\/li>\n<li> Sanz De Galdeano Equiza  Carlos (vocal)<\/li>\n<li>Christian Montenat (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Pedro Alfaro Garcia Se ha realizado un analisis de la evolucion geodinamica de la cuenca durante la [&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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