Basement evolution of the Sierra de la Ventana Fold Belt: new evidence for Cambrian continental rifting along the southern margin of Gondwana

U-Pb sensitive high-resolution ion microprobe data together with geochemical and Nd isotope analyses obtained in the basement complex of the Sierra de la Ventana Fold Belt indicate that the Early Palaeozoic passive margin history of the basin followed Cambrian magmatism related to rifting in a 600 M...

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Bibliographic Details
Main Authors: Rapela, Carlos W, Pankhurst, Robert J, Fanning, Christopher, Grecco, L
Format: Article in Journal/Newspaper
Language:unknown
Published: Geological Society of London 2015
Subjects:
Online Access:http://hdl.handle.net/1885/86057