One of the major retroarc volcanic provinces in the southern Central Andes (34° and 37°S) is developed in the Andean foothills of the San Rafael region between the orogenic front and foreland basement uplifts of Late Miocene age. Here we present the first comprehensive geochronological study of the Quaternary volcanism, previously dated mainly on the basis of stratigraphy. The new unspiked K-Ar radiometric and two radiocarbon determinations encompass many volcanic centers, most of them monogenetic and of basaltic composition exposed between 34° and 35°30′S. The data constrains the basaltic volcanism to between ~ 1.8 Ma and the Holocene. The spatiotemporal distribution of the ages indicates that eruption in the retroarc was episodic with som...
The Antilla magmatic complex (26°10′S, 64°40′W, NW Argentina) attests to magma eruption at ca. 4.7 M...
The hinterland zone of the North Patagonian Andes between 41° and 43°S constitutes a poorly explored...
Late Oligocene to Pliocene magmatism at the latitudes of Malargüe and Chos Malal fold and thrust bel...
A series of mesosilicic volcanic centers have been studied on the San Rafael Block (SRB), 300 km to ...
The Southern Volcanic Zone of the Andes has a Quaternary basaltic province along the retroarc which ...
This work analyzes through field, geophysical, geochemical and geochronological data, a particular s...
The Antilla magmatic complex (26°10′S, 64°40′W, NW Argentina) attests to magma eruption at ca. 4.7 M...
The southern Central Andes recorded retroarc shortening, basin evolution, and magmatic arcmigration ...
Mid-Cenozoic widespread arc magmatism in North Patagonia extends from the forearc to the retroarc zo...
The present contribution describes and analyses the spatial–temporal distribution and main features ...
A Miocene to Pliocene (13 to 4.6 Ma) mostly pyroclastic sequence is exposed along the Iglesia Valley...
Back-arc volcanism in the western Argentinian provinces of Mendoza and Neuquen has been widespread f...
Variable geodynamic contexts have been registered throughout the Cenozoic in the southern Central an...
The Payenia Basaltic Province (PBP) is the largest and the northernmost of the Quaternary back-arc P...
Geologic mapping, together with 73 new K-Ar and ⁴⁰Ar/³⁹Ar age determinations of 45 samples from 17 d...
The Antilla magmatic complex (26°10′S, 64°40′W, NW Argentina) attests to magma eruption at ca. 4.7 M...
The hinterland zone of the North Patagonian Andes between 41° and 43°S constitutes a poorly explored...
Late Oligocene to Pliocene magmatism at the latitudes of Malargüe and Chos Malal fold and thrust bel...
A series of mesosilicic volcanic centers have been studied on the San Rafael Block (SRB), 300 km to ...
The Southern Volcanic Zone of the Andes has a Quaternary basaltic province along the retroarc which ...
This work analyzes through field, geophysical, geochemical and geochronological data, a particular s...
The Antilla magmatic complex (26°10′S, 64°40′W, NW Argentina) attests to magma eruption at ca. 4.7 M...
The southern Central Andes recorded retroarc shortening, basin evolution, and magmatic arcmigration ...
Mid-Cenozoic widespread arc magmatism in North Patagonia extends from the forearc to the retroarc zo...
The present contribution describes and analyses the spatial–temporal distribution and main features ...
A Miocene to Pliocene (13 to 4.6 Ma) mostly pyroclastic sequence is exposed along the Iglesia Valley...
Back-arc volcanism in the western Argentinian provinces of Mendoza and Neuquen has been widespread f...
Variable geodynamic contexts have been registered throughout the Cenozoic in the southern Central an...
The Payenia Basaltic Province (PBP) is the largest and the northernmost of the Quaternary back-arc P...
Geologic mapping, together with 73 new K-Ar and ⁴⁰Ar/³⁹Ar age determinations of 45 samples from 17 d...
The Antilla magmatic complex (26°10′S, 64°40′W, NW Argentina) attests to magma eruption at ca. 4.7 M...
The hinterland zone of the North Patagonian Andes between 41° and 43°S constitutes a poorly explored...
Late Oligocene to Pliocene magmatism at the latitudes of Malargüe and Chos Malal fold and thrust bel...