| Reference Type | Journal (article/letter/editorial) |
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| Title | The formation of a diffusion reaction skarn by pure thermal metamorphism (With Plates I and II.) |
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| Journal | Mineralogical Magazine and Journal of the Mineralogical Society |
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| Authors | Kennedy, W. Q. | Author |
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| Year | 1959 (March) | Volume | 32 |
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| Issue | 244 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_32/32-244-26.pdf+ |
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| DOI | doi:10.1180/minmag.1959.032.244.04 |
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| Generate Citation Formats |
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| Mindat Ref. ID | 5493 | Long-form Identifier | mindat:1:5:5493:9 |
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| GUID | 0 |
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| Full Reference | Kennedy, W. Q. (1959) The formation of a diffusion reaction skarn by pure thermal metamorphism (With Plates I and II.) Mineralogical Magazine and Journal of the Mineralogical Society, 32 (244) 26-31 doi:10.1180/minmag.1959.032.244.04 |
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| Plain Text | Kennedy, W. Q. (1959) The formation of a diffusion reaction skarn by pure thermal metamorphism (With Plates I and II.) Mineralogical Magazine and Journal of the Mineralogical Society, 32 (244) 26-31 doi:10.1180/minmag.1959.032.244.04 |
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| In | (1959) Mineralogical Magazine Vol. 32 (244) Mineralogical Society |
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| Abstract/Notes | SummaryVeins and nodules of cornstone, enclosed in sandstone, have reacted to the thermal influence of a Tertiary dolerite dyke by the development of a wollastonite reaction skarn. This can be shown to have formed as a result of pseudomorphous replacement of the quartz grains by wollastonite, due to outward diffusion of calcium. The process is believed to have taken place at the inversion temperature of quartz (573° C.). |
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