| Reference Type | Journal (article/letter/editorial) |
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| Title | Magnetite–apatite intrusions and calc-alkaline magmatism, Camsell River, N.W.T. |
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| Journal | Canadian Journal of Earth Sciences |
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| Authors | Badham, J. P. N. | Author |
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| Morton, R. D. | Author |
| Year | 1976 (February 1) | Volume | 13 |
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| Issue | 2 |
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| Publisher | Canadian Science Publishing |
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| DOI | doi:10.1139/e76-037Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 474803 | Long-form Identifier | mindat:1:5:474803:2 |
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| GUID | 0 |
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| Full Reference | Badham, J. P. N., Morton, R. D. (1976) Magnetite–apatite intrusions and calc-alkaline magmatism, Camsell River, N.W.T. Canadian Journal of Earth Sciences, 13 (2) 348-354 doi:10.1139/e76-037 |
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| Plain Text | Badham, J. P. N., Morton, R. D. (1976) Magnetite–apatite intrusions and calc-alkaline magmatism, Camsell River, N.W.T. Canadian Journal of Earth Sciences, 13 (2) 348-354 doi:10.1139/e76-037 |
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| In | (1976, February) Canadian Journal of Earth Sciences Vol. 13 (2) Canadian Science Publishing |
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| Abstract/Notes | The Camsell River area comprises a roof pendant of volcanic rocks within an Aphebian (~1800 m.y.) orogenic belt. Magnetite–apatite intrusions and related bodies are common and are closely associated with plutons of intermediate composition. The magnetitic intrusions are interpreted as immiscible liquids that separated from a magma of intermediate composition. The immiscible fractions were predominantly crystalline when they reached their present higher levels, and final emplacement was facilitated by volatile-streaming and fluidization. Their presence in the orogenic belt is taken as further support for the hypothesis that the orogen was of Andean type. |
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