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LAYER SILICATES FROM SERPENTINITE-PEGMATITE CONTACT (WIRY, LOWER SILESIA, POLAND) (1993)
This paper is about a highly tectonized contact between serpentinite and younger pegmatite in the magnesite mine of Wiry that contains various layer silicates.
Reference:
Clays and Clay Minerals, Vol. 41, No. 6, 693-701, 1993.
Clays and Clay Minerals, Vol. 41, No. 6, 693-701, 1993.
Organization:
Institute of Geochemistry, Mineralogy and Petrography, Faculty of Geology
Poland
Institute of Geochemistry, Mineralogy and Petrography, Faculty of Geology
Poland
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