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Structural overprint of a late Paleozoic accretionary system in north-central Chile (34°-35°S) during post-accretional deformation
(Servicio Nacional de Geología y Minería (SERNAGEOMIN), 2009)
G'day Gondwana - the final accretion of a supercontinent: U-Pb ages from the post-orogenic Sao Vicente Granite, northern Paraguay Belt, Brazil
(ELSEVIER SCIENCE BVAMSTERDAM, 2012)
The Paraguay Belt in central South America is part of a larger chain of orogenic belts, including the Araguaia Belt to the northeast and potentially the Pampean Belt to the south, which are believed to mark the suture zone ...
Tectono-sedimentary history of marine forearc basins linked to the evolution of the south central chilean margin (33?30Æ-37?S); insights from seismic data and analogue simulations.
(2010)
The origin and tectono-sedimentary development of marine forearc basins on both, slope and shelf, is strongly linked to the evolution of material transfer at a convergent margin and consequently with the morphology of ...
EVOLUTION OF THE ARCHEAN-EARLY PROTEROZOIC TRANSITION IN THE UNITED STATESEVOLUTION OF THE ARCHEAN-EARLY PROTEROZOIC TRANSITION IN THE UNITED STATES
(Sociedade Brasileira de Geologia, 2018)
The age and tectonic setting of the Puncoviscana Formation in northwestern Argentina: An accretionary complex related to Early Cambrian closure of the Puncoviscana Ocean and accretion of the Arequipa-Antofalla block
(Pergamon-Elsevier Science Ltd, 2011-12)
TIMS and SHRIMP U-Pb zircon geochronology of selected parts of the Puncoviscana Formation suggest its deposition took place mainly during the Early Cambrian, coeval with 540-535. Ma calc-alkaline Pampean arc volcanism ...
Active Deformation, Uplift and Subsidence in Southern South America Throughout the Quaternary: A General Review About Their Development and Mechanisms
(Springer, 2016)
A broad range of processes act today and have acted simultaneously during the Quaternary, producing relief from the Chilean coast, where the Pacific Ocean floor is sinking underneath the South American margin, to the ...