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Provenance variations in the Late Paleozoic accretionary complex of central Chile as indicated by detrital zircons
(Elsevier, 2013)
We present detrital zircon U\Pb SHRIMP age patterns for the central segment (34–42°S) of an extensive accretionary
complex along coastal Chile together with ages for some relevant igneous rocks. The complex consists
of ...
Detrital-zircon U-Pb geochronology of the Quebrada del Carrizo Metamorphic Complex and El Jardin Schists and spatially-related granitoids of the Sierra Castillo Batholith
(Servicio Nacional Geología Minerva, 2015)
U-Pb detrital-zircon geochronology of two discrete outcrops of mica schists of the western border of the Domeyko Cordillera in the Region of Atacama, northern Chile, indicates that the maximum age of sedimentation of their ...
Depositional age and provenance in the San Luis Formation, Sierras Pampeanas, Argentina: Evidence from detrital zircon studies
(Elsevier Ltd, 2019)
The San Luis Formation is one of the lithostratigraphic units constituting the early Paleozoic crystalline basement of the Sierras de San Luis, which are part of the Sierras Pampeanas of central Argentina. The low-grade ...
Lost Terranes of Zealandia: possible development of late Paleozoic and early Mesozoic sedimentary basins at the southwest Pacific margin of Gondwanaland, and their destination as terranes in southern South America
(Servicio Nacional de Geología y Minería (SERNAGEOMIN), 2010)
Further detrital zircon evidence for peri-Gondwanan blocks in the central Appalachian Piedmont Province, USA
(Canadian Science Publishing, 2019)
SHRIMP U-Pb ages of detrital zircons from the early Proterozoic Contendas-Mirante supracrustal belt, Francisco Craton, Bahia, Brazil
(1994)
SHRIMP U-Pb geochronology has been undertaken on detrital zircons in a orthoconglomerate from the metamorphosed Contendas-Mirante supracrustal belt, São Francisco Craton, Bahia, Brazil. The majority of the U-Pb age ...
Geology and U-Pb detrital zircon geochronology coupled with zircon fission tracks of the Jauru formation of Parecis Basin, Brazil
(2021-01-01)
The Jauru Formation fills a symmetric NNW-trending graben whose basement is represented by Calymmian granitic intrusions and the paleoprotorezoic and mesoproterozoic metavolcanic sequence of the Jauru Terrane. The graben ...
Detrital zircon ages of Neoproterozoic sedimentary successions in Uruguay and Argentina: Insights into the geological evolution of the Río de la Plata Craton
(Elsevier Science, 2008-11)
Although the Río de la Plata craton is exposed over a relatively large area in Uruguay, eastern Argentina, and southernmost Brazil, its geological evolution is poorly known because of great geological complexity and paucity ...