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The E-MORB like geochemical features of the Early Paleozoic mafic-ultramafic belt of the Cuyania terrane, western Argentina
(Elsevier, 2013-08)
The Argentine Precordillera is located in the central western region of Argentina, within the Central Andes. Throughout its westernmost sector, mafic and ultramafic bodies including serpentinites, mafic granulites, ...
Major and trace elements in a granulite facies metagabbro from the Proterozoic high grade terrain of Guaxupe, southeastern Brazil, and the nature of the mantle source
(E Schweizerbartsche VerlagsStuttgartAlemanha, 2000)
AGE AND COMPOSITION OF THE GRÃO PARÁ GROUP VOLCANICS, SERRA DOS CARAJÁSAGE AND COMPOSITION OF THE GRÃO PARÁ GROUP VOLCANICS, SERRA DOS CARAJÁS
(Sociedade Brasileira de Geologia, 2018)
Ordovician Volcanism in the Puna (Argentina)
(Nova Publisher Inc, 2020)
In the Central Andes is located one of the major Ordovician basins with fully developed stratigraphic records from Lower Tremadoc to Hirmantian (485-442Ma). As part of this main basin, in the NW of Argentina, the high ...
The Late Pliocene mafic lavas from the Camusú Aike volcanic field (∼50°S, Argentina): Evidence for geochemical variability in slab window magmatism
(Pergamon-Elsevier Science Ltd, 2005-01)
The Camusu Aike volcanic field (CAVF), part of the discontinuous N–S-trending belt of Cenozoic mafic lava formations that occur in a backarc position along extra-Andean Patagonia, is located in southern Patagonia (w508S, ...
The late Eocene–early Miocene El Maitén Belt evolution: Magmatic response to the changing subduction zone geodynamics
(Pergamon-Elsevier Science Ltd, 2020-11)
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 ...