{"id":94189,"date":"2018-03-11T10:13:50","date_gmt":"2018-03-11T10:13:50","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/subsidencia-por-disolucion-de-evaporitas-y-halocinesis-en-el-anticlinal-de-barbastro-y-el-valle-del-rio-cardener-cuenca-terciaria-del-ebro\/"},"modified":"2018-03-11T10:13:50","modified_gmt":"2018-03-11T10:13:50","slug":"subsidencia-por-disolucion-de-evaporitas-y-halocinesis-en-el-anticlinal-de-barbastro-y-el-valle-del-rio-cardener-cuenca-terciaria-del-ebro","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/geomorfologia\/subsidencia-por-disolucion-de-evaporitas-y-halocinesis-en-el-anticlinal-de-barbastro-y-el-valle-del-rio-cardener-cuenca-terciaria-del-ebro\/","title":{"rendered":"Subsidencia por disoluci\u00f3n de evaporitas y halocinesis en el anticlinal de barbastro y el valle del rio cardener (cuenca terciaria del ebro)"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Pedro Lucha L\u00f3pez <\/strong><\/h2>\n<p>En esta tesis doctoral se ha llevado a cabo una cartograf\u00eda geomorfol\u00f3gica del n\u00facleo evapor\u00edtico del anticlinal de barbastro-balaguer entre los valles del cinca y del segre y del tramo final del valle del r\u00edo cardener. en este trabajo se han documentado por primera vez aluviones engrosados por subsidencia k\u00e1rstica sinsedimentaria en los sistemas aluviales de lo reguer, noguera ribagorzana, farfanya y segre. Por otro lado se han documentado basculamientos hacia los m\u00e1rgenes del valle en varias terrazas elaboradas por los r\u00edos cinca y noguera ribagorzana. En el presente trabajo se ha interpretado que estos basculamientos han sido causados por la migraci\u00f3n de la halita la fm. Barbastro hacia el eje de los valles debida a la descarga motivada por el encajamiento de los sistemas fluviales. la cartograf\u00eda geomorfol\u00f3gica del valle del r\u00edo cardener ha revelado que donde este r\u00edo atraviesa las estructuras anticlinales de cardona y suria se localizan una serie de anomal\u00edas que podr\u00edan indicar un aumento en la pendiente del valle del r\u00edo cardener causado por el crecimiento haliocin\u00e9tico de estas estructuras. Por otro lado se han descrito por primera vez engrosamientos y deformaciones causadas por subsidencia k\u00e1rstica en dep\u00f3sitos del cardener y su afluente la riera del tordell en las inmediaciones de suria. Adem\u00e1s, la tasa de ocurrencia de dolinas en el afloramiento de sal de cardona entre 1990 y el a\u00f1o 2004 duplica a la tasa calculada para el a\u00f1o 1989-1990. Este incremento se debe a la entrada de agua procedente del r\u00edo cardener en una mina subterr\u00e1nea de sal en enero de 1999.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Subsidencia por disoluci\u00f3n de evaporitas y halocinesis en el anticlinal de barbastro y el valle del rio cardener (cuenca terciaria del ebro)<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Subsidencia por disoluci\u00f3n de evaporitas y halocinesis en el anticlinal de barbastro y el valle del rio cardener (cuenca terciaria del ebro) <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Pedro Lucha L\u00f3pez <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Zaragoza<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 19\/06\/2009<\/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>Francisco Guti\u00e9rrez Santolalla<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Jos\u00e9 Mar\u00eda Garcia ruiz <\/li>\n<li>eul\u00ed\u00a0lia Masana closa (vocal)<\/li>\n<li>\u00e1ngel Mart\u00edn-serrano Garc\u00eda (vocal)<\/li>\n<li>Jos\u00e9 Mar\u00eda Calaforra chordi (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Pedro Lucha L\u00f3pez En esta tesis doctoral se ha llevado a cabo una cartograf\u00eda geomorfol\u00f3gica del n\u00facleo [&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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