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Infrastructure and provenance of Ganderia: Evidence from detrital zircon ages in the Brookville terrane, southern New Brunswick, Canada.

Authors :
Barr, Sandra M.
White, Chris E.
Davis, Donald W.
McClelland, William C.
van Staal, Cees R.
Source :
Precambrian Research. Jun2014, Vol. 246, p358-370. 13p.
Publication Year :
2014

Abstract

Highlights: [•] Brookville terrane represents ca. 650Ma passive margin of Puncoviscana Ocean. [•] Formed on Proto-Andean-Caribbean edge of Amazonia. [•] Dominated by Meso- and Paleoproterozoic detrital zircon ages. [•] Active margin in Late Neoproterozoic-Cambrian. [•] Separated in mid-Cambrian to become the foundation of Ganderia. [Copyright &y& Elsevier]

Details

Language :
English
ISSN :
03019268
Volume :
246
Database :
Academic Search Index
Journal :
Precambrian Research
Publication Type :
Academic Journal
Accession number :
95827966
Full Text :
https://doi.org/10.1016/j.precamres.2014.03.022