Analysis of high-density current deposits in the Puente Formation (Arequipa Basin), Southern Peru

Descripción del Articulo

The sedimentary Basins of the Jurassic half-superior of the Andes Power stations (Peru), with a rate of high sedimentation, they happened during a period of distension. The Arequipa Basin that was developed during the Jurassic one inferior to half, it presents characteristic morphological, sedimento...

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Detalles Bibliográficos
Autor: Jacay Huarache, Javier Pablo
Formato: artículo
Fecha de Publicación:2005
Institución:Universidad Nacional Mayor de San Marcos
Repositorio:Revistas - Universidad Nacional Mayor de San Marcos
Lenguaje:español
OAI Identifier:oai:ojs.csi.unmsm:article/709
Enlace del recurso:https://revistasinvestigacion.unmsm.edu.pe/index.php/iigeo/article/view/709
Nivel de acceso:acceso abierto
Materia:Sedimentology
megaturbidites
Basin sedimentary
Jurassic
Sedimentología
Megaturbiditas
Cuenca sedimentaria
Jurásico
Descripción
Sumario:The sedimentary Basins of the Jurassic half-superior of the Andes Power stations (Peru), with a rate of high sedimentation, they happened during a period of distension. The Arequipa Basin that was developed during the Jurassic one inferior to half, it presents characteristic morphological, sedimentológicas and tectonic that is typical of a «basin in distension.» One of these characteristics is the turbidityc filler those that present flows of graveness of exceptional thickness Megaturbidites, those that correspond to products of catastrophic events during the resedimentación.
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