{"id":138307,"date":"2026-01-12T17:34:22","date_gmt":"2026-01-12T17:34:22","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/paleomagnetisme-a-les-unitats-sudpirinenques-superiors-implicacions-estructurals\/"},"modified":"2026-01-12T17:34:22","modified_gmt":"2026-01-12T17:34:22","slug":"paleomagnetisme-a-les-unitats-sudpirinenques-superiors-implicacions-estructurals","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/paleomagnetisme-a-les-unitats-sudpirinenques-superiors-implicacions-estructurals\/","title":{"rendered":"Paleomagnetisme a les unitats sudpirinenques superiors. implicacions estructurals"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Jaume Dinares Turell <\/strong><\/h2>\n<p>En este trabajo se han analizado paleomagneticamente diversas litolog\u00edas de edad comprendida entre el jurasico y el oligoceno que afloran en las unidades cabalgantes sudpirenaicas superiores. El objetivo principal es la obtencion y cuantificacion de posibles rotaciones segun el eje vertical en esas unidades. Paralelamente tambien se ha estudiado la relacion entre la deformacion y la fabrica magnetica de las rocas.  el estudio de 152 estaciones ha evidenciado la existencia de rotaciones diferenciales entre las diversas unidades estructurales y dentro de una misma unidad. A grandes rasgos, se ha definido una zona central en la unidad sudpirenaica central donde no se detectan rotaciones subtanciales que permiten la aplicacion de las tecnicas de compensacion y restitucion de cortes geologicos en este sector (p. E. El corte ecors). En cambio, los extremos de las unidades presentan rotaciones que no superan, en general, los 45 grados. Las rotaciones levogiras se situan en el extremo oriental y se pueden asociar a zonas de rampa oblicua levogira y las rotaciones horarias se localizan en el extremo occidental asociadas a rampas dextrogiras.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Paleomagnetisme a les unitats sudpirinenques superiors. implicacions estructurals<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Paleomagnetisme a les unitats sudpirinenques superiors. implicacions estructurals <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Jaume Dinares Turell <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Barcelona<\/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>Pere Santanach Prat<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Enric Banda Tarradellas <\/li>\n<li>Marisa Osete (vocal)<\/li>\n<li>Jim Briden (vocal)<\/li>\n<li>Andr\u00e9s Pocovi Juan (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Jaume Dinares Turell En este trabajo se han analizado paleomagneticamente diversas litolog\u00edas de edad comprendida entre el [&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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