Cryptocrystalline magnesite in weathering crust of ultrabasic rocks

Cryptocrystalline magnesite in weathering crust of ultrabasic rocks Specifics of the morphology, qualitative composition, and spatial extent of cryptocrystalline (pelitomorphic) magnesite deposits and manifestations confined in the weathering crust of ultrabasic rocks are described. It is noted that despite not very big resources, the magnesite material extracted from these deposits can be used for products with high technological properties that are in great demand. In this context, in prospecting minerals associated with ultrabasic rocks (chromites, nickel silicate), it seems expedient to pay special attention to the possibility of discovering industrial-scale deposits of magnesite in the weathering crust of these rocks, especially in vein rocks. Refractories and Industrial Ceramics Springer Journals

Cryptocrystalline magnesite in weathering crust of ultrabasic rocks

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Kluwer Academic Publishers-Consultants Bureau
Copyright © 2006 by Springer Science+Business Media, Inc.
Materials Science; Characterization and Evaluation of Materials; Materials Science, general; Ceramics, Glass, Composites, Natural Materials
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