{"id":10180,"date":"1996-01-01T00:00:00","date_gmt":"1996-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/1996\/01\/01\/estratigrafia-y-bioestratigrafia-conodontos-del-silurico-superior-carbonifero-inferior-del-pirineo-oriental-y-central\/"},"modified":"1996-01-01T00:00:00","modified_gmt":"1996-01-01T00:00:00","slug":"estratigrafia-y-bioestratigrafia-conodontos-del-silurico-superior-carbonifero-inferior-del-pirineo-oriental-y-central","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/estratigrafia-y-bioestratigrafia-conodontos-del-silurico-superior-carbonifero-inferior-del-pirineo-oriental-y-central\/","title":{"rendered":"Estratigrafia y bioestratigrafia (conodontos) del silurico superior-carbonifero inferior del pirineo oriental y central."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Javier Sanz Lopez <\/strong><\/h2>\n<p>La tesis referida constituye un trabajo excelente que aporta datos e interpretaciones sobre diferentes aspectos estratigraficos, paleontologicos y sedimentologicos del paleozoico pirenaico.El estudio paleontologico-sistematico incluye mas de doscientos taxones de conodontos donde destaca la definicion de una especie nueva, icriodus tumulasus. La bioestratigrafia basada en conodontos es utilizado para la atribucion de edad de las unidades litoestratigraficas y la definicion de dos formaciones nuevas. Con el esquema estratigrafico obtenido y las asociaciones de facies diferenciadas se ha construido un esquema de la evolucion de la sedimentacion en el espacio y en el tiempo, para el manto del cadi. Asi como una correlacion con el resto del pirineo, moutoudet y montagne noirec. Dicho esquema de correlacion es utilizado para proponer una subdivision en ciclos sedimentarios de la sucesion estratigrafica entre el silurico superior y el viseense (carbonifero inferior).<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Estratigrafia y bioestratigrafia (conodontos) del silurico superior-carbonifero inferior del pirineo oriental y central.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Estratigrafia y bioestratigrafia (conodontos) del silurico superior-carbonifero inferior del pirineo oriental y central. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Javier Sanz Lopez <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Barcelona<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1996<\/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>Josep Serra Kiel<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Jenaro Luis Garcia Alcalde Fernandez <\/li>\n<li> Sarmiento Chiesa Graciela Noemi (vocal)<\/li>\n<li>Marie-france Perret (vocal)<\/li>\n<li>Francesc Calvet Rovira (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Javier Sanz Lopez La tesis referida constituye un trabajo excelente que aporta datos e interpretaciones sobre diferentes [&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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