Geochemistry of heavy minerals and U–Pb detrital zircon geochronology in the Manantiales Basin: Implications for Frontal Cordillera uplift and foreland basin connectivity in the Andes of central Argentina

The Manantiales Foreland Basin, located at ~ 32°15′S in the Frontal Cordillera, Argentina, contains the sedimentary record of erosion of igneous basement and Miocene volcanic rocks exhumed during the Andean orogeny. U–Pb ages of detrital zircons from the basin fill succession (Chinches Formation) co...

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Detalles Bibliográficos
Autores principales: Pinto, L., Alarcón, P., Morton, A., Naipauer, M.
Formato: JOUR
Materias:
Amphibole
Clinopyroxene
La Ramada
Miocene
Provenance
Andean orogeny
Cenozoic
clinopyroxene
connectivity
cordillera
fold and thrust belt
foreland basin
geochemistry
geochronology
heavy mineral
metavolcanic rock
Paleozoic
Proterozoic
provenance
sedimentary basin
sedimentary rock
Triassic
uplift
uranium-lead dating
volcanic arc
volcanic rock
Andes
Argentina
Comarca Lagunera
Mexico [North America]
Acceso en línea:http://hdl.handle.net/20.500.12110/paper_00310182_v492_n_p104_Pinto
Aporte de:
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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