The Cerro Durazno Pluton belongs to a suite of Paleozoic granitoid intrusions in NW-Argentina, that are central for understanding the tectonic setting of the western margin of Gondwana in Ordovician and Silurian times. The pluton and its host rocks were tectonically overprinted by metamorphic mineral shape fabrics formed under middle greenschist-facies metamorphic conditions and associated with the nearby Agua Rosada Shear Zone. Kinematic analysis of the shear zone based on the geometric relationship between individual segments of the shear plane and principal axes of mineral fabric ellipsoids indicates reverse-sense of shear with a minor component of left-lateral displacement. This is compatible with the kinematics of other ductile deforma...
The basement rock of the Pampean flat-slab (Sierras Pampeanas) in the Central Andes was uplifted and...
The Sierra de Pie de Palo of northwest Argentina preserves middle to lower crustal metamorphic rocks...
The basement rock of the Pampean flat-slab (Sierras Pampeanas) in the Central Andes was uplifted and...
The Cerro Durazno, Brealito, and Cobres granitoid plutons belong to the eastern Ordovician magmatic ...
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...
New structural data from a mid-crustal segment in the Eastern Sierras Pampeanas, coupled with geochr...
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...
Superposed structural fabrics in the easternmost Fuegian Andes reveal two distinct, non-coaxial defo...
Geological, petrological and structural observations were obtained along a 30-km-long traverse acros...
The Sierra Ballena Shear Zone (SBSZ) is part of a high-strain transcurrent system that divides the N...
The Northern and Eastern Sierras Pampeanas in north central Argentina, are uplifted basement blocks ...
The evolution of the Early Palaeozoic orogen of West Gondwana in the Cambrian to Ordovician basement...
The continental protomargin of Western Gondwana in South America records an important Early-Middle O...
The basement rock of the Pampean flat-slab (Sierras Pampeanas) in the Central Andes was uplifted and...
The Sierra de Pie de Palo of northwest Argentina preserves middle to lower crustal metamorphic rocks...
The basement rock of the Pampean flat-slab (Sierras Pampeanas) in the Central Andes was uplifted and...
The Cerro Durazno, Brealito, and Cobres granitoid plutons belong to the eastern Ordovician magmatic ...
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...
New structural data from a mid-crustal segment in the Eastern Sierras Pampeanas, coupled with geochr...
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...
Superposed structural fabrics in the easternmost Fuegian Andes reveal two distinct, non-coaxial defo...
Geological, petrological and structural observations were obtained along a 30-km-long traverse acros...
The Sierra Ballena Shear Zone (SBSZ) is part of a high-strain transcurrent system that divides the N...
The Northern and Eastern Sierras Pampeanas in north central Argentina, are uplifted basement blocks ...
The evolution of the Early Palaeozoic orogen of West Gondwana in the Cambrian to Ordovician basement...
The continental protomargin of Western Gondwana in South America records an important Early-Middle O...
The basement rock of the Pampean flat-slab (Sierras Pampeanas) in the Central Andes was uplifted and...
The Sierra de Pie de Palo of northwest Argentina preserves middle to lower crustal metamorphic rocks...
The basement rock of the Pampean flat-slab (Sierras Pampeanas) in the Central Andes was uplifted and...