{"id":87299,"date":"2000-12-11T00:00:00","date_gmt":"2000-12-11T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/el-karst-litoral-en-el-levante-de-mallorca-una-aproximacion-al-conocimiento-de-su-morfogenesis-y-cronologa%c2%ada\/"},"modified":"2000-12-11T00:00:00","modified_gmt":"2000-12-11T00:00:00","slug":"el-karst-litoral-en-el-levante-de-mallorca-una-aproximacion-al-conocimiento-de-su-morfogenesis-y-cronologa%c2%ada","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/geomorfologia\/el-karst-litoral-en-el-levante-de-mallorca-una-aproximacion-al-conocimiento-de-su-morfogenesis-y-cronologa%c2%ada\/","title":{"rendered":"El karst litoral en el levante de mallorca: una aproximaci\u00f3n al conocimiento de su morfog\u00e9nesis y cronolog\u00eda."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Joaquin Gines Gracia <\/strong><\/h2>\n<p>Se aborda el estudio del karst litoral en la mitad oriental de mmallorca, acometi\u00e9ndolo desde una perspectiva pluridiciplinar que se ocupa tanto de diferentes aspectos de su modelado epigeo (lapiaz costero, cals y barrancos&#8230;) como, sobre todo, de la speculiaridades del rico endokarst existente en el \u00e1rea estudiada.  las investigaciones se han centrado en el an\u00e1lisis de las interferencias entre el dodelado endok\u00e1rtico y la din\u00e1mica litoral, aport\u00e1ndose datos novedosos sobre materias tan variadas como: la geoqu\u00edmica de las aguas fre\u00e1ticas litorales, la morfog\u00e9nesis de las caviddes subterr\u00e1neas, los rellenos aut\u00f3ctonos y al\u00f3ctonos de las cavernas costeras, y la evoluci\u00f3n del endokarst estudiado a lo largo del plio-cuaternario.  el mayor inter\u00e9s de los trabajados realizados radica en las valiosas informaciones crono-estraigr\u00e1ficas obtenidas en relaci\u00f3n con las oscilaciones pleistoc\u00e9nicas del nivel marino. En concreto, el estudio de los espeleotemas fre\u00e1ticos ha mostrado que \u00e9stos constituyen un excelente registro de la historia del nivel del mediterr\u00e1nero, durante el pleistoceno medio y superior y el holoceno. Este tipo de dep\u00f3sitos secundarios propios de las cuevas k\u00e1rsticas litorales han sido estudiados mediante diversas t\u00e9ncias (dataciones radiom\u00e9tricas th\/u, mediciones de est, microscop\u00eda \u00f3ptica y lectr\u00f3nica, an\u00e1lisis de is\u00f3topos estables &#8230;) Con vistas a la obtenci\u00f3n de datos cronol\u00f3gicos y paleoclim\u00e1ticos precisos. De particualr relevancia son las curvas eut\u00e1ticas propuestas par los \u00faltimos 300ka, en el mediterr\u00e1neo occidentas, las cualaes presentan un detalle fuera de los com\u00fan en el rango de edad comprendido entre 150 y 50 ka. B.P.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>El karst litoral en el levante de mallorca: una aproximaci\u00f3n al conocimiento de su morfog\u00e9nesis y cronolog\u00eda.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 El karst litoral en el levante de mallorca: una aproximaci\u00f3n al conocimiento de su morfog\u00e9nesis y cronolog\u00eda. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Joaquin Gines Gracia <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Illes balears<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 12\/11\/2000<\/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  Jos\u00e9 Forn\u00f3s Ast\u00f3<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: vicen\u00ed\u00a7 m. Rossell\u00f3 verger <\/li>\n<li>Juan  Jos\u00e9 Dur\u00e1n valsero (vocal)<\/li>\n<li>paola Tuccimei (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 Joaquin Gines Gracia Se aborda el estudio del karst litoral en la mitad oriental de mmallorca, acometi\u00e9ndolo [&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":[3498,14353,5741,75,19034],"tags":[169936,35368,39212,169935,182783,26821],"class_list":["post-87299","post","type-post","status-publish","format-standard","hentry","category-aguas-subterraneas","category-geocronologia-y-radioisotopos","category-geografia-fisica","category-geomorfologia","category-illes-balears","tag-joaquin-gines-gracia","tag-jose-maria-calaforra-chordi","tag-juan-jose-duran-valsero","tag-juan-jose-fornos-asto","tag-paola-tuccimei","tag-viceni-m-rossello-verger"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/87299","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=87299"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/87299\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=87299"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=87299"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=87299"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}