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Infrastructure and provenance of Ganderia: Evidence from detrital zircon ages in the Brookville terrane, southern New Brunswick, Canada.
- 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]
- Subjects :
- *PROVENANCE (Geology)
*ZIRCON
*CAMBRIAN Period
*PROTEROZOIC Era
Subjects
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