The 2.5 Ga Duxbury massif, Quebec : a remobilized piece of pre-3.0 Ga sialic basement(?)
The Duxbury massif, Eastmain District, Quebec, is a complex tonalitic intrusion that is internally divisible into a homogeneous border zone of granodiorite (Rb–Sr total-rock isochron age = 2500 ± 85 Ma; initial 87 Sr/ 86 Sr = 0.7023 ± 0.0003) and a heterogeneous core zone of tonalite (Rb–Sr total-ro...
Published in: | Canadian Journal of Earth Sciences |
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Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Canadian Science Publishing
1980
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Subjects: | |
Online Access: | http://dx.doi.org/10.1139/e80-001 http://www.nrcresearchpress.com/doi/pdf/10.1139/e80-001 |