| Reference Type | Journal (article/letter/editorial) |
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| Title | Lherzolite nodules from a Pleistocene cinder cone in central Yukon |
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| Journal | Canadian Journal of Earth Sciences |
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| Authors | Sinclair, P. D. | Author |
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| Tempelman-Kluit, D. J. | Author |
| Medaris Jr., L. G. | Author |
| Year | 1978 (February 1) | Volume | 15 |
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| Issue | 2 |
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| Publisher | Canadian Science Publishing |
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| DOI | doi:10.1139/e78-022Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 475727 | Long-form Identifier | mindat:1:5:475727:0 |
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| GUID | 0 |
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| Full Reference | Sinclair, P. D., Tempelman-Kluit, D. J., Medaris Jr., L. G. (1978) Lherzolite nodules from a Pleistocene cinder cone in central Yukon. Canadian Journal of Earth Sciences, 15 (2) 220-226 doi:10.1139/e78-022 |
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| Plain Text | Sinclair, P. D., Tempelman-Kluit, D. J., Medaris Jr., L. G. (1978) Lherzolite nodules from a Pleistocene cinder cone in central Yukon. Canadian Journal of Earth Sciences, 15 (2) 220-226 doi:10.1139/e78-022 |
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| In | (1978, February) Canadian Journal of Earth Sciences Vol. 15 (2) Canadian Science Publishing |
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| Abstract/Notes | Fresh spinel lherzolite nodules occur in basaltic tuff on the flank of a Pleistocene cinder cone built on Selkirk Lavas in central Yukon. The nodules are mineralogically and chemically similar to others from diverse localities. The texture and mineral chemistry are consistent with an upper mantle origin for the Selkirk nodules. Equilibration temperatures for the nodules have been determined to be about 1100 °C. |
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