| Reference Type | Journal (article/letter/editorial) |
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| Title | An erosional structure in a layered dolerite dyke, West Greenland |
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| Journal | Geological Magazine |
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| Authors | Williams, H. R. | Author |
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| Year | 1976 (January) | Volume | 113 |
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| Issue | 1 |
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| Publisher | Cambridge University Press (CUP) |
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| DOI | doi:10.1017/s001675680004303xSearch in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 251115 | Long-form Identifier | mindat:1:5:251115:7 |
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| GUID | 0 |
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| Full Reference | Williams, H. R. (1976) An erosional structure in a layered dolerite dyke, West Greenland. Geological Magazine, 113 (1) 77-82 doi:10.1017/s001675680004303x |
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| Plain Text | Williams, H. R. (1976) An erosional structure in a layered dolerite dyke, West Greenland. Geological Magazine, 113 (1) 77-82 doi:10.1017/s001675680004303x |
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| In | (1976, January) Geological Magazine Vol. 113 (1) Cambridge University Press (CUP) |
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| Abstract/Notes | SummaryA vertical channel structure within a layered dolerite dyke resulted from differential magmatic flow. Layering in both dyke and channel is formed of more feldspathic dolerite attributed to fluctuations in water vapour pressure and supercooling during crystallization. |
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These are possibly similar items as determined by title/reference text matching only.
