Skip navigation
Skip navigation

Ediacaran to Lower Ordovician age for rocks ascribed to the Schist-Graywacke Complex (Iberian Massif, Spain): Evidence from detrital zircon SHRIMP U-Pb geochronology

Talavera, C.; Montero, P.; Martínez Poyatos, D.; Williams, Ian


New SHRIMP U-Pb ages of detrital zircon obtained from eight samples of Neoproterozoic to Lower Paleozoic graywackes, schists, microconglomerates and shales provide the maximum depositional age and a new zircon age pattern for the Schist-Graywacke Complex

CollectionsANU Research Publications
Date published: 2012
Type: Journal article
Source: Gondwana Research
DOI: 10.1016/


File Description SizeFormat Image
01_Talavera_Ediacaran_to_Lower_Ordovician_2012.pdf3.82 MBAdobe PDF    Request a copy

Items in Open Research are protected by copyright, with all rights reserved, unless otherwise indicated.

Updated:  19 May 2020/ Responsible Officer:  University Librarian/ Page Contact:  Library Systems & Web Coordinator