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Evolution of exhumationand erosion in western west gondwanaland as recorded by detrital zircons of late Neoproterozoic and Cambrian sedimentary rocks of NW and Centraal Argentina.
(Springer-Verlag, 2011-06)
The evolution of the provenance areas for Late Neoproterozoic,Cambrian and Early Ordovician sedimentary and meta-sedimentaryrocks of north central and northwest Argentina is discussed using 123maximum ages of detrital ...
Detrital zircons U-Pb SHRIMP ages and provenance of La Modesta Formation, Patagonia Argentina
(Elsevier, 2013)
This paper summarizes the geology of the Paleozoic La Modesta Formation in Patagonia, Argentina, and
presents new SHRIMP UePb dating of detrital zircons from muscovite-chlorite schist and tourmalinite.
Also complementary ...
Detrital zircon age patterns and provenance of the metamorphic complexes of southern chile
(PERGAMON-ELSEVIER SCIENCE LTD,, 2003)
Provenance variations in the late paleozoic accretionary complex of central chile as indicated by detrital zircons
(INTERNATIONAL ASSOCIATION FOR GONDWANA RESEARCH, DEPARTMENT OF GEOSCIENCE, 2013)
Detrital zircons u-pb shrimp ages and provenance of la modesta formation, patagonia argentina
(PERGAMON-ELSEVIER SCIENCE LTD, 2013)
Detrital zircons from late paleozoic accretionary complexes in north-central chile (28 degrees-32 degrees s): possible fingerprints of the chilenia terrane
(PERGAMON-ELSEVIER SCIENCE LTD,, 2011)
Detrital zircons from late paleozoic accretionary complexes in north-central chile (28 degrees-32 degrees s): possible fingerprints of the chilenia terrane
(PERGAMON-ELSEVIER SCIENCE LTD,, 2011)
On the presence of Upper Paleocene rocks in the foreland succession at Cabo Nariz, Tierra del Fuego, Chile: geology and new palynological and U-Pb data
(Servicio Nacional de Geología y Minería (SERNAGEOMIN), 2010)
Isotopic studies on detrital zircons of Silurian-Devonian siliciclastic sequences from Argentinean North Patagonia and Sierra de la Ventana regions: comparative provenance
(Springer, 2011-12)
The Silurian-Devonian siliciclastic sedimentary units known as Sierra Grande Formation and the upper part of the Ventana Group crop out in the eastern area of the North Patagonian Massif and in the Ventania system, toward ...