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Reynolds, P. H., Kublick, E. E., Muecke, G. K. (1973) Potassium–Argon Dating of Slates from the Meguma Group, Nova Scotia. Canadian Journal of Earth Sciences, 10 (7) 1059-1067 doi:10.1139/e73-091

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Reference TypeJournal (article/letter/editorial)
TitlePotassium–Argon Dating of Slates from the Meguma Group, Nova Scotia
JournalCanadian Journal of Earth Sciences
AuthorsReynolds, P. H.Author
Kublick, E. E.Author
Muecke, G. K.Author
Year1973 (July 1)Volume10
Issue7
PublisherCanadian Science Publishing
DOIdoi:10.1139/e73-091Search in ResearchGate
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Mindat Ref. ID473760Long-form Identifiermindat:1:5:473760:9
GUID0
Full ReferenceReynolds, P. H., Kublick, E. E., Muecke, G. K. (1973) Potassium–Argon Dating of Slates from the Meguma Group, Nova Scotia. Canadian Journal of Earth Sciences, 10 (7) 1059-1067 doi:10.1139/e73-091
Plain TextReynolds, P. H., Kublick, E. E., Muecke, G. K. (1973) Potassium–Argon Dating of Slates from the Meguma Group, Nova Scotia. Canadian Journal of Earth Sciences, 10 (7) 1059-1067 doi:10.1139/e73-091
In(1973, July) Canadian Journal of Earth Sciences Vol. 10 (7) Canadian Science Publishing
Abstract/Notes Recent reconstructions of the geologic evolution of Atlantic Canada based on plate-tectonic models have aroused new interest in the timing of orogenic events on both sides of the Atlantic. K–Ar apparent ages ranging from 332–403 m.y. are reported for 15 whole-rock slate and hornfels samples from the Halifax Formation of the Meguma Group. Four biotite concentrates from spatially associated granitic intrusions yield K–Ar ages of 364–369 m.y. A minimum age of about 390 m.y. for the regional metamorphic event is deduced from the whole-rock slate data. Granitic intrusion at approximately 367 m.y. profoundly affected the argon clock in many Halifax slates and resulted in its partial resetting even in slates which do not display mineralogic or textural effects of superimposed thermal metamorphism. The 390 m.y. minimum age for regional metamorphism supports suggestions by other workers that the currently widely-accepted 395 m.y. date for the Devonian–Silurian boundary may need revision.


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