Thermochronologic Evidence for Late Eocene Andean Mountain Building at 30°S

The Andes between 28° and 30°S represent a transition between the Puna-Altiplano Plateau and the Frontal/Principal Cordillera fold-and-thrust belts to the south. While significant early Cenozoic deformation documented in the Andean Plateau, deciphering the early episodes of deformation during Andean...

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Detalles Bibliográficos
Autores principales:	Lossada, A.C., Giambiagi, L., Hoke, G.D., Fitzgerald, P.G., Creixell, C., Murillo, I., Mardonez, D., Velásquez, R., Suriano, J.
Formato:	JOUR
Materias:	Eocene constructional phase exhumation mountain building South Central Andes thermochronology Cooling Deformation Fission reactions Inverse problems Landforms Phosphate minerals Tectonics Central Andes Exhumation Mountain building Thermochronology Geochronology cooling deformation Eocene fold and thrust belt mountain region stress Andes
Acceso en línea:	http://hdl.handle.net/20.500.12110/paper_02787407_v36_n11_p2693_Lossada
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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