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1.- Detrital-zircon geochronology demonstrates common provenance of Cambrian-Devonian sandstones of the Cuyania (greater Precordillera) Terrane of western Argentina and Neoproterozoic sandstones deposited on the Rio de La Plata Craton of Uruguay and eastern Argentina
Geological Society of America (GSA); Boulder, CO; USA; United States, 2006
Geological Society of America, 2006 annual meeting
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