Metamorphic Differentiation of Talc-Magnesite-Chlorite Rocks in Shetland
- 1 April 1952
- journal article
- research article
- Published by Cambridge University Press (CUP) in Geological Magazine
- Vol. 89 (2) , 97-105
- https://doi.org/10.1017/s0016756800067431
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.Keywords
This publication has 6 references indexed in Scilit:
- Thetford, Disraeli, and eastern half of Warwick map-areas, QuebecPublished by Natural Resources Canada/CMSS/Information Management ,1937
- The Metamorphic Geology of Unst in the Shetland IslandsQuarterly Journal of the Geological Society, 1934
- Hydrothermal metamorphism of an ultrabasic intrusive at Schuyler, VirginiaAmerican Journal of Science, 1933
- On quartz-kyanite-rocks in Unst, Shetland Islands, and their bearing on metamorphic differentiationMineralogical Magazine and Journal of the Mineralogical Society, 1933
- Origin of the Vermont talc deposits, with a discussion on the formation of talc in generalEconomic Geology, 1927
- The Serpentines and Associated Rocks and Minerals of the Shetland IslandsQuarterly Journal of the Geological Society, 1927