| Reference Type | Journal (article/letter/editorial) |
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| Title | An Eocene Rb–Sr isochron for rhyolite plugs, Skukum area, Yukon Territory |
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| Journal | Canadian Journal of Earth Sciences |
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| Authors | Pride, Monica J. | Author |
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| Clark, George S. | Author |
| Year | 1985 (November 1) | Volume | 22 |
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| Issue | 11 |
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| Publisher | Canadian Science Publishing |
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| DOI | doi:10.1139/e85-184Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 478481 | Long-form Identifier | mindat:1:5:478481:8 |
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| GUID | 0 |
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| Full Reference | Pride, Monica J., Clark, George S. (1985) An Eocene Rb–Sr isochron for rhyolite plugs, Skukum area, Yukon Territory. Canadian Journal of Earth Sciences, 22 (11) 1747-1753 doi:10.1139/e85-184 |
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| Plain Text | Pride, Monica J., Clark, George S. (1985) An Eocene Rb–Sr isochron for rhyolite plugs, Skukum area, Yukon Territory. Canadian Journal of Earth Sciences, 22 (11) 1747-1753 doi:10.1139/e85-184 |
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| In | (1985, November) Canadian Journal of Earth Sciences Vol. 22 (11) Canadian Science Publishing |
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| Abstract/Notes | A new Rb–Sr whole-rock isochron for the Skukum rhyolite is 53.3 ± 1.1 Ma with an initial ratio of 0.7053. The rhyolite forms small plugs spatially and probably genetically related to the Skukum volcanic complex in the southwestern Yukon. They were intruded into granitic rocks of the Coast Plutonic Belt. The intrusions are coeval and part of an Eocene plutonic, subvolcanic, and volcanic suite correlated with the Bennett Lake cauldron complex. The initial 87Sr/86Sr ratio matches interpretations of the tectonic evolution of Yukon Crystalline Terrane and Coast Plutonic Complex. |
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