| Reference Type | Journal (article/letter/editorial) |
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| Title | 'Residence' Contamination of K, Rb, Li, and Tl in Diabase Dikes |
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| Journal | Canadian Journal of Earth Sciences |
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| Authors | Fratta, M. | Author |
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| Shaw, Denis M. | Author |
| Year | 1974 (March 1) | Volume | 11 |
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| Issue | 3 |
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| Publisher | Canadian Science Publishing |
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| DOI | doi:10.1139/e74-038Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 474032 | Long-form Identifier | mindat:1:5:474032:6 |
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| GUID | 0 |
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| Full Reference | Fratta, M., Shaw, Denis M. (1974) 'Residence' Contamination of K, Rb, Li, and Tl in Diabase Dikes. Canadian Journal of Earth Sciences, 11 (3) 422-429 doi:10.1139/e74-038 |
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| Plain Text | Fratta, M., Shaw, Denis M. (1974) 'Residence' Contamination of K, Rb, Li, and Tl in Diabase Dikes. Canadian Journal of Earth Sciences, 11 (3) 422-429 doi:10.1139/e74-038 |
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| In | (1974, March) Canadian Journal of Earth Sciences Vol. 11 (3) Canadian Science Publishing |
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| Abstract/Notes | A diabase dike of the Mackenzie swarm has been sampled at two localities where it intrudes basic volcanics and granite respectively. The portion of the dike intruding the granite has statistically significant higher contents of K, Rb, Li, and Tl, as a result of in situ, residence, contamination from the country rock. Ion transfer from the granite toward the diabase took place mainly before the magma crystallized, therefore a process of differentiation was superimposed to that of diffusion. |
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