| Reference Type | Journal (article/letter/editorial) |
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| Title | Paragonite paragenesis from the garnet granulites of the Jijal complex, Kohistan, N. Pakistan |
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| Journal | Mineralogical Magazine | ISSN | 0026-461X |
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| Authors | Jan, M. Q. | Author |
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| Wilson, R. N. | Author |
| Windley, B. F. | Author |
| Year | 1982 | Volume | 45 |
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| Issue | 337 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_45/45-337-73.pdf+ |
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| DOI | doi:10.1180/minmag.1982.045.337.08Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 3318 | Long-form Identifier | mindat:1:5:3318:7 |
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| GUID | 0 |
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| Full Reference | Jan, M. Q., Wilson, R. N., Windley, B. F. (1982) Paragonite paragenesis from the garnet granulites of the Jijal complex, Kohistan, N. Pakistan. Mineralogical Magazine, 45 (337) 73-77 doi:10.1180/minmag.1982.045.337.08 |
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| Plain Text | Jan, M. Q., Wilson, R. N., Windley, B. F. (1982) Paragonite paragenesis from the garnet granulites of the Jijal complex, Kohistan, N. Pakistan. Mineralogical Magazine, 45 (337) 73-77 doi:10.1180/minmag.1982.045.337.08 |
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| In | (1982) Mineralogical Magazine Vol. 45 (337) Mineralogical Society |
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| Abstract/Notes | AbstractChemistry of six white micas from the high-pressure garnet granulites of Jijal is presented, together with trace elements, refractive indices, and 2Vα for one. The micas are rich in the paragonite component (over 93%), with one analysis having the highest 100 Na/(Na + K) ratio (98.5) so far reported. The paragonite is not a stable mineral of the granulites but was overprinted on the granulites at about 505–540°C and 8–9 kbar (suggesting a depth of 30 km). |
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