| Reference Type | Journal (article/letter/editorial) |
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| Title | Myrmekite and muscovite developed by retrograde metamorphism at Broken Hill, New South Wales |
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| Journal | Mineralogical Magazine |
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| Authors | Phillips, Evan R. | Author |
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| Ransom, D. M. | Author |
| Vernon, R. H. | Author |
| Year | 1972 (March) | Volume | 38 |
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| Issue | 297 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_38/38-297-570.pdf+ |
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| DOI | doi:10.1180/minmag.1972.038.297.05Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 6532 | Long-form Identifier | mindat:1:5:6532:4 |
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| GUID | 0 |
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| Full Reference | Phillips, Evan R., Ransom, D. M., Vernon, R. H. (1972) Myrmekite and muscovite developed by retrograde metamorphism at Broken Hill, New South Wales. Mineralogical Magazine, 38 (297) 570-578 doi:10.1180/minmag.1972.038.297.05 |
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| Plain Text | Phillips, Evan R., Ransom, D. M., Vernon, R. H. (1972) Myrmekite and muscovite developed by retrograde metamorphism at Broken Hill, New South Wales. Mineralogical Magazine, 38 (297) 570-578 doi:10.1180/minmag.1972.038.297.05 |
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| In | (1972, March) Mineralogical Magazine Vol. 38 (297) Mineralogical Society |
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| Abstract/Notes | SummaryRetrograde metamorphism of gneisses and pegmatites leads in part to the destruction of feldspar and its replacement by late-stage lobate myrmekite and muscovite. Reactions promoted by retrogression suggest a range in volume of quartz production that may supplement that developed by exsolution and lead to deviations from the strict proportionality relationship suggested by previous workers. There is no need, however, to propose that quartz in myrmekite originates by constriction of pre-existing quartz within exsolved albite. |
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