| Reference Type | Journal (article/letter/editorial) |
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| Title | Talc-kyanite-quartz schists and other high-pressure assemblages from Zambia |
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| Journal | Mineralogical Magazine |
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| Authors | Vrána, S. | Author |
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| Barr, M. W. C. | Author |
| Year | 1972 (September) | Volume | 38 |
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| Page(s) | 837-846 | Issue | 299 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_38/38-299-837.pdf+ |
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| DOI | doi:10.1180/minmag.1972.038.299.07Search in ResearchGate |
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| Mindat Ref. ID | 6587 | Long-form Identifier | mindat:1:5:6587:4 |
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| GUID | 217eef86-150d-4c35-a31c-cede61802ab8 |
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| Full Reference | Vrána, S., Barr, M. W. C. (1972) Talc-kyanite-quartz schists and other high-pressure assemblages from Zambia. Mineralogical Magazine, 38 (299) 837-846 doi:10.1180/minmag.1972.038.299.07 |
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| Plain Text | Vrána, S., Barr, M. W. C. (1972) Talc-kyanite-quartz schists and other high-pressure assemblages from Zambia. Mineralogical Magazine, 38 (299) 837-846 doi:10.1180/minmag.1972.038.299.07 |
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| In | (1972, September) Mineralogical Magazine Vol. 38 (299) Mineralogical Society |
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| Abstract/Notes | SummaryTalc-kyanite-quartz schists, Mg-chlorite-kyanite-quartz schists, kyanite gedritites, and kyanite-bronzite gedritites occur in the Central Province of Zambia. Experimental work in the system MgO-Al2O3-SiO2-H2O suggests that these assemblages formed at pressures in excess of 10 kb. |
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