| Autor: |
Komarova, G. N., Moleva, V. A., Rudnitskaya, E. S., Dmitriyeva, M. T. |
| Zdroj: |
International Geology Review; February 1968, Vol. 10 Issue: 2 p135-142, 8p |
| Abstrakt: |
Accumulations of fine platy crystals of bavenite, colorless or white, often with inclusions of graphite, were discovered in an albitized garnet skarn, in a geological environment in which the mineral, a relatively high-temperature metasomatic replacer of phenacite and feldspar, is definitely not an end-stage product of a hydrothermal process. - IGR Staff. |
| Databáze: |
Supplemental Index |
| Externí odkaz: |
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