The geodynamic evolution of the proto-Andean margin of Gondwana during the Paleozoic was characterized by repeated subduction processes associated with the docking of several terranes, including the Cuyania–Precordillera terrane and the Chilenia terrane, and the development of the calc–alkaline Famatinian continental magmatic arc. In the Sierra de La Huerta (30°56′–31°29′ S and 67°17′–67°32′ W), at the southwestern end of the Western Sierras Pampeanas, some mafic to ultramafic igneous bodies belonging to the Famatinian arc were affected by regional metamorphism of the medium-pressure granulite facies (7–7.5 kbar, ≈ 850 °C). After this regional metamorphism, local mylonitization under amphibolite facies along discrete NW–SE to NNW–SSE striki...
The rocks of Sierra de Maz and Sierra del Espinal (Western Sierras Pampeanas) represent pre-Famatini...
This magmatism is principally developed in N W Argentina, with some prolongations in the neighbour c...
Fil: Rapela, Carlos Washington. Centro de Investigaciones Geológicas (CIG). Facultad de Ciencias Nat...
The geodynamic evolution of the proto-Andean margin of Gondwana during the Paleozoic was characteriz...
The geodynamic evolution of the proto-Andean margin of Gondwana during the Paleozoic was characteriz...
The geodynamic evolution of the proto-Andean margin of Gondwana during the Paleozoic was characteriz...
Two Early Paleozoic orogenic cycles in the Gondwana margin of NW Argentina were driven by subduction...
From a detailed study of a 500 km transect in the Sierras Pampeanas, central-west Argentina, two pre...
Geological, petrological and structural observations were obtained along a 30-km-long traverse acros...
This thesis investigated the evolution of a high temperature, low pressure crustal block of the Late...
The Cerro Durazno Pluton belongs to a suite of Paleozoic granitoid intrusions in NW-Argentina, that ...
This thesis investigated the evolution of a high temperature, low pressure crustal block of the Late...
The Cerro Durazno, Brealito, and Cobres granitoid plutons belong to the eastern Ordovician magmatic ...
The rocks of Sierra de Maz and Sierra del Espinal (Western Sierras Pampeanas) represent pre-Famatini...
Metasedimentary high-pressure upper amphibolite facies gneisses (1.2 ± 0.1. GPa and 780 ± 45 °C) at ...
The rocks of Sierra de Maz and Sierra del Espinal (Western Sierras Pampeanas) represent pre-Famatini...
This magmatism is principally developed in N W Argentina, with some prolongations in the neighbour c...
Fil: Rapela, Carlos Washington. Centro de Investigaciones Geológicas (CIG). Facultad de Ciencias Nat...
The geodynamic evolution of the proto-Andean margin of Gondwana during the Paleozoic was characteriz...
The geodynamic evolution of the proto-Andean margin of Gondwana during the Paleozoic was characteriz...
The geodynamic evolution of the proto-Andean margin of Gondwana during the Paleozoic was characteriz...
Two Early Paleozoic orogenic cycles in the Gondwana margin of NW Argentina were driven by subduction...
From a detailed study of a 500 km transect in the Sierras Pampeanas, central-west Argentina, two pre...
Geological, petrological and structural observations were obtained along a 30-km-long traverse acros...
This thesis investigated the evolution of a high temperature, low pressure crustal block of the Late...
The Cerro Durazno Pluton belongs to a suite of Paleozoic granitoid intrusions in NW-Argentina, that ...
This thesis investigated the evolution of a high temperature, low pressure crustal block of the Late...
The Cerro Durazno, Brealito, and Cobres granitoid plutons belong to the eastern Ordovician magmatic ...
The rocks of Sierra de Maz and Sierra del Espinal (Western Sierras Pampeanas) represent pre-Famatini...
Metasedimentary high-pressure upper amphibolite facies gneisses (1.2 ± 0.1. GPa and 780 ± 45 °C) at ...
The rocks of Sierra de Maz and Sierra del Espinal (Western Sierras Pampeanas) represent pre-Famatini...
This magmatism is principally developed in N W Argentina, with some prolongations in the neighbour c...
Fil: Rapela, Carlos Washington. Centro de Investigaciones Geológicas (CIG). Facultad de Ciencias Nat...