During Mid-Cenozoic times, voluminous and genetically heterogeneous volcanism took place across North Patagonia in response to a period of plate tectonic reorganization. One of these volcanic associations is represented by the El Maitén Belt, located to the east of the main Andes for over ~300 km. This volcanic belt reflects the evolution of a continental arc in an extensional setting with remarkable compositional variations between the late Eocene and the early Miocene. We present new field and isotopic data that, together with lithological, geochronological and geochemical data compilations, suggest significant changes in the nature and location of magmatic sources. This evolution may be summarized in three stages: i) incipient arc magmat...
The Somún Curá Magmatic Province (SCMP) is a Cenozoic volcanic region comprised by several basaltic ...
The magmatic history and tectonic evolution of the Valle del Cura region has received the attention ...
Geochemical variations in arc- and within-plate magmatic associations since Late Cretaceous times ar...
Voluminous Paleogene magmatic rocks (44 to 29 Ma) are found in a retroarc position in the Northern P...
Mid-Cenozoic widespread arc magmatism in North Patagonia extends from the forearc to the retroarc zo...
The influence of tectonic processes in evolution of magmatic suitesevaluated through their geochemic...
Variable geodynamic contexts have been registered throughout the Cenozoic in the southern Central an...
Late Oligocene to Pliocene magmatism at the latitudes of Malargüe and Chos Malal fold and thrust bel...
The tectonic regime associated with the Oligo-Miocene Cura-Mallín Formationand equivalents in the Ma...
The Catán Lil Basin is an intermontane basin developed on the wedge top of the Miocene North Patagon...
Late Cretaceous-early Paleocene magmatism at Southern Central Andes is represented by incomplete and...
Miocene sedimentary successions of the Ñirihuau and Collón Cura formations east of the El Maitén Bel...
Geochemical and geochronological data reveal that late Oligocene-early Miocene time is a break point...
The Oligocene to present evolution of the North Patagonian Andes is analyzed linking geological and ...
The hinterland zone of the North Patagonian Andes between 41° and 43°S constitutes a poorly explored...
The Somún Curá Magmatic Province (SCMP) is a Cenozoic volcanic region comprised by several basaltic ...
The magmatic history and tectonic evolution of the Valle del Cura region has received the attention ...
Geochemical variations in arc- and within-plate magmatic associations since Late Cretaceous times ar...
Voluminous Paleogene magmatic rocks (44 to 29 Ma) are found in a retroarc position in the Northern P...
Mid-Cenozoic widespread arc magmatism in North Patagonia extends from the forearc to the retroarc zo...
The influence of tectonic processes in evolution of magmatic suitesevaluated through their geochemic...
Variable geodynamic contexts have been registered throughout the Cenozoic in the southern Central an...
Late Oligocene to Pliocene magmatism at the latitudes of Malargüe and Chos Malal fold and thrust bel...
The tectonic regime associated with the Oligo-Miocene Cura-Mallín Formationand equivalents in the Ma...
The Catán Lil Basin is an intermontane basin developed on the wedge top of the Miocene North Patagon...
Late Cretaceous-early Paleocene magmatism at Southern Central Andes is represented by incomplete and...
Miocene sedimentary successions of the Ñirihuau and Collón Cura formations east of the El Maitén Bel...
Geochemical and geochronological data reveal that late Oligocene-early Miocene time is a break point...
The Oligocene to present evolution of the North Patagonian Andes is analyzed linking geological and ...
The hinterland zone of the North Patagonian Andes between 41° and 43°S constitutes a poorly explored...
The Somún Curá Magmatic Province (SCMP) is a Cenozoic volcanic region comprised by several basaltic ...
The magmatic history and tectonic evolution of the Valle del Cura region has received the attention ...
Geochemical variations in arc- and within-plate magmatic associations since Late Cretaceous times ar...