The Miocene stratigraphy of the Laberinto area (Río Ica Valley) and its bearing on the geological history of the East Pisco Basin (south-central Peru)

JAB received funding from the United States Geological Survey , Climate Research and Development Program , for this study. DO was supported by CONCYTEC (Peru) research grants CB ( N° 105-2018 - FONDECYT ) and “Incorporación de Investigadores” ( N° E038-2019-02-FONDECYT-BM ). RE was supported by Geos...

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Detalles Bibliográficos
Autores: DeVries T.J., Barron J.A., Urbina-Schmitt M., Ochoa D., Esperante R., Snee L.W.
Tipo de recurso: artículo
Fecha de publicación:2021
País:Perú
Institución:Consejo Nacional de Ciencia Tecnología e Innovación
Repositorio:CONCYTEC-Institucional
Idioma:inglés
OAI Identifier:oai:repositorio.concytec.gob.pe:20.500.12390/3064
Acceso en línea:https://hdl.handle.net/20.500.12390/3064
https://doi.org/10.1016/j.jsames.2021.103458
Access Level:acceso abierto
Palabra clave:Pisco formation
Chilcatay formation
Diatoms
East Pisco Basin
Miocene
Olistostrome
Peru
https://purl.org/pe-repo/ocde/ford#2.07.01
Descripción
Sumario:JAB received funding from the United States Geological Survey , Climate Research and Development Program , for this study. DO was supported by CONCYTEC (Peru) research grants CB ( N° 105-2018 - FONDECYT ) and “Incorporación de Investigadores” ( N° E038-2019-02-FONDECYT-BM ). RE was supported by Geosciences Research Institute grant GRI19-1 . LWS was supported as an employee of the United States Geological Survey during the 1980s. TJD and MU did not receive any grant from funding agencies in the public, commercial, or not-for-profit sectors.