The tectonic regime associated with the Oligo-Miocene Cura-Mallín Formationand equivalents in the Main Andean Cordillera between 35° and 40° S, theVentana and Abanico formations to the south and north, respectively, is still matter of debate. While most authors have agreed in relating them to an extensional regime that could have interrupted Andean orogenesis, others have provided evidence of coexistence with an ongoing compressional regime at least for the upper part of their record. Available geochronological, structural, geochemical, thermochronological, and basin subsidence data between 33° and 43° S are compiled and analyzed in this chapter in order to provide a tectonic framework for these rocks. Based on this analysis, two different ...
The Catán Lil Basin is an intermontane basin developed on the wedge top of the Miocene North Patagon...
During Mid-Cenozoic times, voluminous and genetically heterogeneous volcanism took place across Nort...
The magmatic history and tectonic evolution of the Valle del Cura region has received the attention ...
The Oligocene to present evolution of the North Patagonian Andes is analyzed linking geological and ...
Miocene sedimentary successions of the Ñirihuau and Collón Cura formations east of the El Maitén Bel...
The hinterland zone of the North Patagonian Andes between 41° and 43°S constitutes a poorly explored...
The distribution and timing of the deformation for the North Patagonian broken foreland is nowadays ...
The Northern Patagonian Andes have been constructed through multiple mechanisms that range from tect...
The Andes between 28° and 30°S represent a transition between the Puna-Altiplano Plateau and the Fro...
The magmatic history and tectonic evolution of the Valle del Cura region has received the attention ...
Several segments of the Central and Southern Andes show deformation evidences located far away from ...
A Miocene to Pliocene (13 to 4.6 Ma) mostly pyroclastic sequence is exposed along the Iglesia Valley...
The Conglomerado Los Patos is a coarse-grained clastic unitthat crops out irregularly in the San Ant...
The interaction of tectonics and climate is considered the main determining factor in the developmen...
One of the main morphological changes along the Southern Central Andes occurs from 36° to 39°S. The ...
The Catán Lil Basin is an intermontane basin developed on the wedge top of the Miocene North Patagon...
During Mid-Cenozoic times, voluminous and genetically heterogeneous volcanism took place across Nort...
The magmatic history and tectonic evolution of the Valle del Cura region has received the attention ...
The Oligocene to present evolution of the North Patagonian Andes is analyzed linking geological and ...
Miocene sedimentary successions of the Ñirihuau and Collón Cura formations east of the El Maitén Bel...
The hinterland zone of the North Patagonian Andes between 41° and 43°S constitutes a poorly explored...
The distribution and timing of the deformation for the North Patagonian broken foreland is nowadays ...
The Northern Patagonian Andes have been constructed through multiple mechanisms that range from tect...
The Andes between 28° and 30°S represent a transition between the Puna-Altiplano Plateau and the Fro...
The magmatic history and tectonic evolution of the Valle del Cura region has received the attention ...
Several segments of the Central and Southern Andes show deformation evidences located far away from ...
A Miocene to Pliocene (13 to 4.6 Ma) mostly pyroclastic sequence is exposed along the Iglesia Valley...
The Conglomerado Los Patos is a coarse-grained clastic unitthat crops out irregularly in the San Ant...
The interaction of tectonics and climate is considered the main determining factor in the developmen...
One of the main morphological changes along the Southern Central Andes occurs from 36° to 39°S. The ...
The Catán Lil Basin is an intermontane basin developed on the wedge top of the Miocene North Patagon...
During Mid-Cenozoic times, voluminous and genetically heterogeneous volcanism took place across Nort...
The magmatic history and tectonic evolution of the Valle del Cura region has received the attention ...