Detrital zircon U–Pb ages of metasedimentary rocks from Sierra de Valle Fértil: Entrapment of Middle and Late Cambrian marine successions in the deep roots of the Early Ordovician Famatinian arc-Reference-Cited by-同舟云学术

Detrital zircon U–Pb ages of metasedimentary rocks from Sierra de Valle Fértil: Entrapment of Middle and Late Cambrian marine successions in the deep roots of the Early Ordovician Famatinian arc

Published:2012-08 Issue: Volume:37 Page:77-94
ISSN:0895-9811
Container-title:Journal of South American Earth Sciences
language:en
Short-container-title:Journal of South American Earth Sciences

Author:

Cristofolini E.A.,Otamendi J.E.,Ducea M.N.,Pearson D.M.,Tibaldi A.M.,Baliani I.

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

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4. The Pacific Gondwana margin in the late Neoproterozoic-early Paleozoic: detrital zircon U-Pb ages from metasediments in northwest Argentina reveal their maximum age, provenance and tectonic setting;Adams;Gondwana Research,2010

5. Ordovician back arc foreland and Ocloyic thrust belt development on the western Gondwana margin as a response to Precodillera terrane accretion;Astini;Tectonics,2004

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