| Reference Type | Journal (article/letter/editorial) |
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| Title | A note on the Quesnel Lake Gneiss, Caribou Mountains, British Columbia |
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| Journal | Canadian Journal of Earth Sciences |
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| Authors | Montgomery, John R. | Author |
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| Ross, John V. | Author |
| Year | 1989 (July 1) | Volume | 26 |
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| Issue | 7 |
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| Publisher | Canadian Science Publishing |
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| DOI | doi:10.1139/e89-128Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 480583 | Long-form Identifier | mindat:1:5:480583:4 |
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| GUID | 0 |
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| Full Reference | Montgomery, John R., Ross, John V. (1989) A note on the Quesnel Lake Gneiss, Caribou Mountains, British Columbia. Canadian Journal of Earth Sciences, 26 (7) 1503-1508 doi:10.1139/e89-128 |
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| Plain Text | Montgomery, John R., Ross, John V. (1989) A note on the Quesnel Lake Gneiss, Caribou Mountains, British Columbia. Canadian Journal of Earth Sciences, 26 (7) 1503-1508 doi:10.1139/e89-128 |
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| In | (1989, July) Canadian Journal of Earth Sciences Vol. 26 (7) Canadian Science Publishing |
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| Abstract/Notes | The Quesnel Lake Gneiss is one of several large bodies of gneiss emplaced into the westernmost exposure of the Hadrynian to Paleozoic(?) metasedimentary rocks of the Snowshoe Group in the Omineca Belt, central British Columbia. The gneiss has a deformational history comparable to that of its enveloping rocks, and isotope studies indicate that its age of emplacement is Late Devonian to Early Mississippian and that its age of synkinematic metamorphism is mid-Jurassic. From petrochemical analyses and structural studies, we interpret the gneiss as being a late Paleozoic igneous intrusion into the probable western margin of the North American craton. |
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