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Fernando Lebinson,Martín Turienzo,Natalia Sánchez,Vanesa Araujo,María Celeste D?Annunzio,Luis Dimieri
Pág. 249 - 273
The Agrio fold and thrust belt is a thick-skinned orogenic belt developed since Late Cretaceous in response to the convergence between the Nazca and South American plates. The integration of new structural field data and seismic line interpretation allow...
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Eduardo Ignacio Moscoso,Eduardo Contreras-Reyes
Pág. 564 - 572
Most of the recent published geodetic models of the 2010 Maule, Chile mega-thrust earthquake (Mw=8.8) show a pronounced slip maximum of 15-20 m offshore Iloca, indicating that co-seismic slip was largest north of the epicenter of the earthquake rupture a...
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Cividini, A. Zenti, C. L.
Pág. 139 - 139
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Dewaikar, D. M.
Pág. 140 - 140
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Nelson Munoz,Reynaldo Charrier,Teresa Jordan
Pág. 55 - 80
A reinterpretation of the structural style on the eastern Cordillera Domeyko and the adjacent Salar de Atacama Basin reveals the existence of west-dipping, high-angle, thrust-faults extending below the Cordillera Domeyko and Cordón de Lila, resulting fro...
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