Metamorphic differentiation of talc-magnesite-chlorite rocks in Shetland
- 97-105p. Illustration
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.
Metamorphic differentiation - Talc rock - Shetland island - Scotland Metamorphic differentiation - Magnesite rock - Shetland island - Scotland Metamorphic differentiation - Chlorite rock - Shetland island - Scotland Petrography - Differented rock - Scotland