{"id":75410,"date":"2005-06-07T00:00:00","date_gmt":"2005-06-07T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/estratigrafa%c2%ada-y-tectonica-del-triasico-sudiberico-en-el-sector-oriental-de-la-cordillera-betica\/"},"modified":"2005-06-07T00:00:00","modified_gmt":"2005-06-07T00:00:00","slug":"estratigrafa%c2%ada-y-tectonica-del-triasico-sudiberico-en-el-sector-oriental-de-la-cordillera-betica","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/estratigrafa%c2%ada-y-tectonica-del-triasico-sudiberico-en-el-sector-oriental-de-la-cordillera-betica\/","title":{"rendered":"Estratigraf\u00eday tect\u00f3nica del tri\u00e1sico sudib\u00e9rico en el sector oriental de la cordillera b\u00e9tica."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Fernando P\u00e9rez Valera <\/strong><\/h2>\n<p>La investigaci\u00f3n se ha centrado en las rocas del tri\u00e1sico que afloran en el sector centro-oriental de la cordillera b\u00e9tica. Se hace un estudio de la estrataigraf\u00eda y tect\u00f3nica de las rocas del tri\u00e1sico sudib\u00e9rico que afloran en las zonas externas de la cordillera. Este trabajo aporta numerosos e interesantes datos sobre el tri\u00e1sico de esta zona, donde apenas se han realizado de este tipo anteriormente y adem\u00e1s, supone un gran avance en el conocimiento del tri\u00e1sico de la cordillera b\u00e9tica.  en esatas rocas del tri\u00e1sico sudib\u00e9rico se han distinguido  las facies germ\u00e1ncias, bustansdstein, muschelkalk y keuper. Tambi\u00e9n se han reconocido los carbonatos de edad noriensse, definidos en el sector central de la cordillera como formaci\u00f3n zamoranos.  en el buntsandstein se define la formaci\u00f3n arroyo molinos, cosntituida principalmente por arcillas rojas y grises, con aresnisca, aunque hacei alas zonas m\u00e1s sur-orientales puede estar formada por yesos. En el muschelkalk se definand os formaciones, que pueden extenderse en todo el \u00e1mbito de la cordillera b\u00e9tica, la formaci\u00f3n siles, que corresponde a lod carbonatos depositados en la \u00e1reas m\u00e1s proximales  del paleomargen sudib\u00e9rico, y la formaci\u00f3n ceheg\u00edn, que est\u00e1 constituida por os carbonatos depositados en las \u00e1reas m\u00e1s distales. Estas formaciones presentan facies de una rampa carbonatada que evoluciona a una plataforma somera, pero siempre en un contexto de un mara epicontinental. En las facies keuper se han distinguido todas las formaciones definidas en el sector central de la cordillera, denominadas abreviadamenta k1, k2, k3 y k4-k5. Se establecen algunas diferencias entre los afloramientos m\u00e1s septentrionale, en el ambito del preb\u00e9tico y los meridionales. En lso carbonatos de edad noriense (formaci\u00f3n zamoranos)se han reconocido los tres miembros caracteristicos definidso en esta formaci\u00f3n. en la mayor\u00eda de los casos aflolora com bloques de una megabrecha yes\u00edfera<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Estratigraf\u00eday tect\u00f3nica del tri\u00e1sico sudib\u00e9rico en el sector oriental de la cordillera b\u00e9tica.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Estratigraf\u00eday tect\u00f3nica del tri\u00e1sico sudib\u00e9rico en el sector oriental de la cordillera b\u00e9tica. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Fernando P\u00e9rez Valera <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Granada<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 06\/07\/2005<\/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> P\u00e9rez L\u00f3pez Alberto Diego<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Juan Fernandez Martinez <\/li>\n<li>leopoldo M\u00e1rquez sanz (vocal)<\/li>\n<li>Carlos Sanz de galdeano (vocal)<\/li>\n<li>Jos\u00e9 L\u00f3pez g\u00f3mez (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Fernando P\u00e9rez Valera La investigaci\u00f3n se ha centrado en las rocas del tri\u00e1sico que afloran en el 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