Reference Type | Journal (article/letter/editorial) |
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Title | Rb/Sr dating of rocks from the Wollaston Lake Belt, Saskatchewan |
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Journal | Canadian Journal of Earth Sciences |
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Authors | Cumming, G. L. | Author |
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Scott, B. P. | Author |
Year | 1976 (February 1) | Volume | 13 |
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Issue | 2 |
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Publisher | Canadian Science Publishing |
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DOI | doi:10.1139/e76-038Search in ResearchGate |
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| Generate Citation Formats |
Mindat Ref. ID | 474805 | Long-form Identifier | mindat:1:5:474805:6 |
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|
GUID | 0 |
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Full Reference | Cumming, G. L., Scott, B. P. (1976) Rb/Sr dating of rocks from the Wollaston Lake Belt, Saskatchewan. Canadian Journal of Earth Sciences, 13 (2) 355-364 doi:10.1139/e76-038 |
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Plain Text | Cumming, G. L., Scott, B. P. (1976) Rb/Sr dating of rocks from the Wollaston Lake Belt, Saskatchewan. Canadian Journal of Earth Sciences, 13 (2) 355-364 doi:10.1139/e76-038 |
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In | (1976, February) Canadian Journal of Earth Sciences Vol. 13 (2) Canadian Science Publishing |
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Abstract/Notes | Rb and Sr measurements on rocks of the Wollaston Lake fold belt in Saskatchewan indicate a major metamorphic resetting of most of the whole-rock Rb/Sr systems, particularly in the arkosic units, associated with the Hudsonian orogeny and dated at 1850 m.y. (λ = 1.39 × 10−11 y−1).Some of the so-called 'young' granites in the area appear to be primary intrusives of that age, but others contain clear evidence of containing older material. A tentative age of 2650 m.y. for the Archean granites is suggested on the basis of three samples that appear to have retained their original Rb/Sr ratios. Two quartzite samples suggest an Archean age of about 2360 m.y. for the sediments in the area although the data are inconclusive. A late metamorphism is well dated at 1730 m.y. by a mineral isochron and by ratios in remobilized material along the edge of the Johnson River batholith. |
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