Reference Type | Journal (article/letter/editorial) |
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Title | THE PETROLOGY OF TWO ZONED SCAPOLITE SKARNS |
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Journal | Canadian Journal of Earth Sciences |
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Authors | Shaw, Denis M. | Author |
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Schwarcz, Henry P. | Author |
Sheppard, Simon M. F. | Author |
Year | 1965 (December 1) | Volume | 2 |
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Issue | 6 |
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Publisher | Canadian Science Publishing |
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DOI | doi:10.1139/e65-043Search in ResearchGate |
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| Generate Citation Formats |
Mindat Ref. ID | 471504 | Long-form Identifier | mindat:1:5:471504:1 |
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GUID | 0 |
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Full Reference | Shaw, Denis M., Schwarcz, Henry P., Sheppard, Simon M. F. (1965) THE PETROLOGY OF TWO ZONED SCAPOLITE SKARNS. Canadian Journal of Earth Sciences, 2 (6) 577-595 doi:10.1139/e65-043 |
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Plain Text | Shaw, Denis M., Schwarcz, Henry P., Sheppard, Simon M. F. (1965) THE PETROLOGY OF TWO ZONED SCAPOLITE SKARNS. Canadian Journal of Earth Sciences, 2 (6) 577-595 doi:10.1139/e65-043 |
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In | (1965, December) Canadian Journal of Earth Sciences Vol. 2 (6) Canadian Science Publishing |
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Abstract/Notes | A spheroidal skarn body at Gib Lake, Pontiac County, Quebec, occurs in phlogopite marble, and shows concentric zones several centimeters thick. The zonal sequence is (a) core of blue scapolite; (b) pargasite–albite intergrowth; (c) pure phlogopite; (d) serpentinized forsterite–dolomite marble. The minerals have been analyzed. A zoned skarn with a similar sequence was found 15 miles south on Calumet Island.Phase assemblages are consistent with upper amphibolite facies metamorphism. The zonal sequence is explained by reaction between a spheroidal quartzo-feldspathic mass and an enveloping dolomitic marble through radial diffusion of Mg (inward) and Si, Al (outward), establishing local equilibrium between adjacent phases. Mg, Al, and Si behaved as phase-determining inert components, Ca was probably in excess, while Na, K, H, Cl, C, F, S were perfectly mobile. |
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