| Reference Type | Journal (article/letter/editorial) |
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| Title | Alkali gabbro fragments in Sudbury breccia |
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| Journal | Canadian Journal of Earth Sciences |
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| Authors | Dupuis, L. | Author |
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| Whitehead, R. E. S. | Author |
| Davies, J. F. | Author |
| Year | 1990 (June 1) | Volume | 27 |
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| Issue | 6 |
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| Publisher | Canadian Science Publishing |
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| DOI | doi:10.1139/e90-079Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 480925 | Long-form Identifier | mindat:1:5:480925:2 |
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| GUID | 0 |
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| Full Reference | Dupuis, L., Whitehead, R. E. S., Davies, J. F. (1990) Alkali gabbro fragments in Sudbury breccia. Canadian Journal of Earth Sciences, 27 (6) 784-786 doi:10.1139/e90-079 |
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| Plain Text | Dupuis, L., Whitehead, R. E. S., Davies, J. F. (1990) Alkali gabbro fragments in Sudbury breccia. Canadian Journal of Earth Sciences, 27 (6) 784-786 doi:10.1139/e90-079 |
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| In | (1990, June) Canadian Journal of Earth Sciences Vol. 27 (6) Canadian Science Publishing |
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| Abstract/Notes | Alkali gabbro fragments in Sudbury breccia have been misinterpreted as potash-enriched greywacke. Because of differing proportions of arenaceous and argillaceous components, greywackes vary widely in chemical composition. However, on plots of SiO2/Al2O3 against TiO2, greywacke-argillites fall along a hyperbolic sorting curve. Alkali gabbro fragments fall well off the curve. The distinction between the two rock types is supported by other chemical data. |
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