Reference Type | Journal (article/letter/editorial) |
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Title | Malayaite and tin-bearing garnet from a skarn at Gumble, NSW, Australia |
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Journal | Mineralogical Magazine | ISSN | 0026-461X |
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Authors | Mulholland, I. R. | Author |
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Year | 1984 (March) | Volume | 48 |
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Issue | 346 |
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Publisher | Mineralogical Society |
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Download URL | https://rruff.info/doclib/MinMag/Volume_48/48-346-27.pdf+ |
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DOI | doi:10.1180/minmag.1984.048.346.04Search in ResearchGate |
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| Generate Citation Formats |
Mindat Ref. ID | 3584 | Long-form Identifier | mindat:1:5:3584:6 |
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|
GUID | 0 |
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Full Reference | Mulholland, I. R. (1984) Malayaite and tin-bearing garnet from a skarn at Gumble, NSW, Australia. Mineralogical Magazine, 48 (346) 27-30 doi:10.1180/minmag.1984.048.346.04 |
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Plain Text | Mulholland, I. R. (1984) Malayaite and tin-bearing garnet from a skarn at Gumble, NSW, Australia. Mineralogical Magazine, 48 (346) 27-30 doi:10.1180/minmag.1984.048.346.04 |
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In | (1984, March) Mineralogical Magazine Vol. 48 (346) Mineralogical Society |
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Abstract/Notes | AbstractMalayaite and tin-bearing garnet occur within a skarn assemblage at Gumble, NSW. A metasomatic origin is proposed for these minerals under conditions of T = 300-500Β°C Xco2 < 0.30 and fO2 = 10β18 to 10β30 bars. Malayaite has formed as a result of reaction between a metasomatic fluid rich in Sn, F, H2O and silica, and tin-bearing andradite and wollastonite. The main requirements for tin-bearing skarn formation appear to be an F-Sn-rich granite, an iron-rich skarn assemblage, and a relatively long cooling history. |
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