Widespread fluid infiltration during metamorphism of the Witwatersrand goldfields: generation of chloritoid and pyrophyllite
- 5 May 1988
- journal article
- Published by Wiley in Journal of Metamorphic Geology
- Vol. 6 (3) , 311-332
- https://doi.org/10.1111/j.1525-1314.1988.tb00423.x
Abstract
No abstract availableKeywords
This publication has 10 references indexed in Scilit:
- Metamorphism of the Witwatersrand gold fields: conditions during peak metamorphismJournal of Metamorphic Geology, 1987
- Hydrothermally altered peraluminous Archaean granites as a provenance model for Witwatersrand sedimentsMineralium Deposita, 1987
- Geochemistry of fluid inclusions from the McIntyre-Hollinger gold deposit, Timmins, Ontario, CanadaEconomic Geology, 1984
- Rare-earth element mobility in alteration pipes below massive CuZn-sulfide depositsChemical Geology, 1984
- Archaean Sedimentary Rocks and Their Relation to the Composition of the Archaean Continental CrustPublished by Springer Nature ,1984
- The Witwatersrand pyrites and metamorphismMineralogical Magazine, 1983
- Calculation of the thermodynamic properties of aqueous silica and the solubility of quartz and its polymorphs at high pressures and temperaturesAmerican Journal of Science, 1977
- Petrogenesis of Metamorphic RocksPublished by Springer Nature ,1976
- The stability of staurolite and chloritoid and their significance in metamorphism of pelitic rocksContributions to Mineralogy and Petrology, 1969
- Hydrothermal origin of the Rand gold deposits; Part 1, Testimony of the conglomeratesEconomic Geology, 1930