Paleoenvironment studies of the Pisco formation: Ocucaje locality

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The Cerro La Bruja outarop included into Pisco Formation related to fosiliferous content (mollusca and vertebrades) get a exactly datation of series, developed by marine sediments interbeded volcanics of volcanic activities from Cordillera occidental and diatomites, related to volcanics activities....

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Detalles Bibliográficos
Autor: Báez Gómez, Diego A.
Formato: artículo
Fecha de Publicación:2006
Institución:Universidad Nacional Mayor de San Marcos
Repositorio:Revistas - Universidad Nacional Mayor de San Marcos
Lenguaje:español
OAI Identifier:oai:ojs.csi.unmsm:article/2770
Enlace del recurso:https://revistasinvestigacion.unmsm.edu.pe/index.php/iigeo/article/view/2770
Nivel de acceso:acceso abierto
Materia:Pisco
Formación
Mioceno medio
Plioceno superior
Estratigrafía
Tectónica
Diatomeas
Formation
Middle miocene
late Pliocene
Stratigraphy
Tectonics
Diatoms
Descripción
Sumario:The Cerro La Bruja outarop included into Pisco Formation related to fosiliferous content (mollusca and vertebrades) get a exactly datation of series, developed by marine sediments interbeded volcanics of volcanic activities from Cordillera occidental and diatomites, related to volcanics activities. In this Formation were found since thousand mile years a huge faune from marine vertebrates. This fauna is well know and it includes fish (selaceous and teleosteous), reptiles (turtles and cocodriles), binds and marine mamiferos (spheniscidae, phocidae). The funistic association shows sedimentary enviromment represent to this litoestratigrafic unit, go from shoreface to onshore, to abundance and good preservation of fosils shows a fast sandy. The tectonic activity in the area is strong and its shows in the variation from sea level (transgressive – regressive) log in the outcrop up shong marks to seven levels of backward from sea level, showing a relationships to sedimentary process.
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