Variable structural controls through time in the Southern Central Andes (~36°S)

The Southern Central Andes at 36°S have been recognized as an orogenic belt where contraction, accommodated mainly by basement structures, is associated with the inversion of a Late Triassic-Early Jurassic extensional detachment. Based on a structural cross-section, constrained by field data, 2D sei...

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Detalles Bibliográficos
Autores principales:	Orts, D.L., Folguera, A., Giménez, M., Ramos, V.A.
Formato:	JOUR
Materias:	Argentina Brittle-ductile transitions Central Andes Foreland basin Malargüe fold and thrust belt Orogenic front Tectonic inversion basement rock deformation extension fold and thrust belt foreland basin geochronology gravity anomaly orogenic belt slip structural geology subduction tectonic evolution upper crust Andes Cordillera Malargue Mendoza Paraguay
Acceso en línea:	http://hdl.handle.net/20.500.12110/paper_07187092_v39_n2_p220_Orts
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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