M. S. Amin
Abstract
Abstract Practically monomineralic masses of talc, of magnesite, and of chlorite are formed in talc-magnesite-chlorite-rocks as a result of localized shearing and associated hydrothermal activity within deformation-belts.
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Abstract Practically monomineralic masses of talc, of magnesite, and of chlorite are formed in talc-magnesite-chlorite-rocks as a result of localized shearing and associated hydrothermal activity within deformation-belts.
Key concepts: Magnesite, Talc, Chlorite, Geology, Geochemistry, Shearing (physics), Metamorphic rock, Hydrothermal circulation