{"id":84133,"date":"2000-07-04T00:00:00","date_gmt":"2000-07-04T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/el-aptiense-albiense-de-karrantza-lanestosa-bizkaia-y-cantabria\/"},"modified":"2000-07-04T00:00:00","modified_gmt":"2000-07-04T00:00:00","slug":"el-aptiense-albiense-de-karrantza-lanestosa-bizkaia-y-cantabria","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/el-aptiense-albiense-de-karrantza-lanestosa-bizkaia-y-cantabria\/","title":{"rendered":"El aptiense-albiense de karrantza-lanestosa (bizkaia y cantabria)"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Miguel Angel Lopez Horgue <\/strong><\/h2>\n<p>Se presentan los resultados obtenidos del estudio estratigr\u00e1fico del aptiense-albiense de la zona de karrantza-lanestosa (bizkaia) y zonas lim\u00edtrofes de cantabria. Los materiales objeto de investigaci\u00f3n alcanzan m\u00e1s de 2000 m de espesor y se dividen en dos conjuntos litol\u00f3gicos principales: calizas conrudistas, margas, lutitas y areniscas. Para el estudio en detalle de estas series se han realizado cartogrf\u00edas a escala 1:25,000 y 1:50,000. como resutlado se han diferenciado 11 unidades litoestraigr\u00e1ficas, 9 in\u00e9ditas y 5 subunidades.As\u00edmismo, se ha identifiado 23 especies de formain\u00edferos y 11 especies de ammonites, siendo la mayor\u00eda de ellas primera cita en la zona y, algunas de ellas, en la cuenca vasco-cant\u00e1brica. La dataci\u00f3n precisa de las series ha permitido la distinci\u00f3n de dos grandes lagunas estratigr\u00e1ficas correspondientes a casi todo el aptiense y a gran parte del albiense medio y superior.  se describen sedimentol\u00f3gicamente 9 sistemas deposicionales; 1, plataforma terr\u00edgena (formaci\u00f3n ereza); 2, plataforma carbonatada (la paredina); 3, plataforma carbonatada (polvor\u00edn); 4, plataforma mixta (miniclara); 5, rampa carbonatada (ventalaperra); 6 plataforma mixta (sangrices); 7, plataforma carbonatada-cuenca (ranero); 8, plataforma mixta (sope\u00f1a); y 9, plataforma terr\u00edgena (la escrita).  loa zona de estudio sufri\u00f3 una comaartimentaci\u00f3n importante durante el aptiense-albiense debido a tect\u00f3nica sin sedimentaria, condicionando la din\u00e1mica de lso distintos sistemas deposicionales. Se han identificado 6 discordancias locales, 1 falla superficial, 3 pliegues y 8 fallas profundas, inferidas en base a criterios estratigr\u00e1ficos y sedimentol\u00f3gicos.Alguna de estas estructuras fue reactivada posteriormente en la orog\u00e9nica alpina, y las mayores fracturas se corresponden con lineaciones estructurales heredadas  de la orogenia herc\u00ednica. Rasgos tect\u00f3nicos y sedimentol\u00f3gicos apoyan un encuadre geodin\u00e1mico de desgarr<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>El aptiense-albiense de karrantza-lanestosa (bizkaia y cantabria)<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 El aptiense-albiense de karrantza-lanestosa (bizkaia y cantabria) <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Miguel Angel Lopez Horgue <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Pa\u00eds vasco\/euskal herriko unibertsitatea<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 07\/04\/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>Joaquin Garc\u00eda Mond\u00e9jar<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: victoriano Pujalte navarro <\/li>\n<li> Mart\u00edn mart\u00edn Jos\u00e9 Manuel (vocal)<\/li>\n<li>Luis Pomar  goma (vocal)<\/li>\n<li>alfonso Melendez hevia (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Miguel Angel Lopez Horgue Se presentan los resultados obtenidos del estudio estratigr\u00e1fico del aptiense-albiense de la zona 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