Whole-Rock Rb/Sr Ages of Metamorphic Rocks from Northern Ellesmere Island, Canadian Arctic Archipelago. I. The Gneiss Terrain between Ayles Fiord and Yelverton Inlet

The first Precambrian ages from the Northern Ellesmere Fold Belt are reported. Six rocks from the largest gneiss terrain in northern Ellesmere Island yield a Late Precambrian age (minimum 742 ± 12 m.y.) of regional metamorphism. Relatively high initial 87 Sr/ 86 Sr suggests that the rocks were deriv...

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Bibliographic Details
Published in:Canadian Journal of Earth Sciences
Main Authors: Sinha, A. K., Frisch, Thomas
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1975
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Online Access:http://dx.doi.org/10.1139/e75-010
http://www.nrcresearchpress.com/doi/pdf/10.1139/e75-010
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Summary:The first Precambrian ages from the Northern Ellesmere Fold Belt are reported. Six rocks from the largest gneiss terrain in northern Ellesmere Island yield a Late Precambrian age (minimum 742 ± 12 m.y.) of regional metamorphism. Relatively high initial 87 Sr/ 86 Sr suggests that the rocks were derived from crustal materials.