Crustal structure of the high Andes in the North Pampean flat slab segment from magnetic and gravity data

The Main Andes at the northern Chilean-Pampean flat slab segment were formed by the inversion of late Oligocene to early Miocene extensional depocenters in Neogene times. Their structure, size and depth are loosely constrained by field data since these sequences have amalgamated forming an almost co...

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Detalles Bibliográficos
Autores principales: Sánchez, M.A., Winocur, D., Álvarez, O., Folguera, A., Martinez, M.P.
Formato: JOUR
Materias:
Aerial magnetic data
Central Andes
Paleogene basin architecture
Paleozoic basement structure.
Satellite gravity data
Terrestrial gravity data
crustal structure
discontinuity
gravity field
magnetic field
Paleozoic
satellite data
slab
three-dimensional modeling
Andes
Acceso en línea:http://hdl.handle.net/20.500.12110/paper_08959811_v73_n_p153_Sanchez
Aporte de:
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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