Sedimentologic and stratigraphic evolution of the Cacheuta basin: Constraints on the development of the Miocene retroarc foreland basin, south-central Andes

Retroarc foreland basins in contractional arc settings contain evidence of temporal and spatial variations in magmatic activity, deformation, and exhumation along the continental margin and serve as excellent recorders of subduction dynamics through time. The Cacheuta basin, northwestern Mendoza Pro...

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Detalles Bibliográficos
Autores principales: Buelow, E.K., Suriano, J., Mahoney, J.B., Kimbrough, D.L., Mescua, J.F., Giambiagi, L.B., Hoke, G.D.
Formato: JOUR
Materias:
Deformation
Geochronology
Petrography
Silicate minerals
Stratigraphy
Zircon
Basin development
Continental margin
Crustal thickenings
Flat-slab subductions
Magmatic activity
Sediment provenance
Subduction dynamics
Temporal and spatial variation
Tectonics
basin evolution
continental margin
crustal thickening
exhumation
foreland basin
Miocene
orogeny
provenance
sedimentology
stratigraphy
subduction zone
thin section
transition zone
uplift
zircon
Andes
Argentina
Cacheuta
Cordillera Frontal
Cordillera Principal
Mendoza
Pampas
Precordillera
Southern Volcanic Zone
Acceso en línea:http://hdl.handle.net/20.500.12110/paper_19418264_v10_n3_p366_Buelow
Aporte de:
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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