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Blaxland, Alan B., Curtis, Laurence W. (1977) Chronology of the Red Wine alkaline province, central Labrador. Canadian Journal of Earth Sciences, 14 (8) 1940-1946 doi:10.1139/e77-164

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Reference TypeJournal (article/letter/editorial)
TitleChronology of the Red Wine alkaline province, central Labrador
JournalCanadian Journal of Earth Sciences
AuthorsBlaxland, Alan B.Author
Curtis, Laurence W.Author
Year1977 (August 1)Volume14
Issue8
PublisherCanadian Science Publishing
DOIdoi:10.1139/e77-164Search in ResearchGate
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Mindat Ref. ID475511Long-form Identifiermindat:1:5:475511:5
GUID0
Full ReferenceBlaxland, Alan B., Curtis, Laurence W. (1977) Chronology of the Red Wine alkaline province, central Labrador. Canadian Journal of Earth Sciences, 14 (8) 1940-1946 doi:10.1139/e77-164
Plain TextBlaxland, Alan B., Curtis, Laurence W. (1977) Chronology of the Red Wine alkaline province, central Labrador. Canadian Journal of Earth Sciences, 14 (8) 1940-1946 doi:10.1139/e77-164
In(1977, August) Canadian Journal of Earth Sciences Vol. 14 (8) Canadian Science Publishing
Abstract/Notes An 11-point Rb–Sr whole-rock isochron for the regionally metamorphosed Red Wine alkaline province gives an age of intrusion of 1345 ± 75 Ma (errors quoted at 2σ) and an initial 87Sr/86Sr ratio of (1.7021 ± 0.0103. Two 5-point mineral isochrons give ages of ~1000 Ma that represent metamorphic 'resetting' of the alkaline rocks. The whole-rock intrusion age compares closely with the early stage of magmatism in the Gardar Province of south Greenland where un-metamorphosed agpaitic igneous rocks, similar to those of the Red Wine Province, occur. In both provinces, alkaline plutonic rocks are associated, both spatially and chronologically, with thick sequences of continental sediments and basaltic lavas, and the new age data lend strong support to the supposition that the Gardar and Red Wine rocks are parts of the same pre-drift magmatic province and inferred rift system. The Gardar Province has, however, escaped the effects of the Grenville regional metamorphism which severely affected the Red Wine rocks.


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