The origins of late-stage rocks in the St Austell granite—a re-interpretation
- 16 May 1984
- journal article
- Published by Geological Society of London in Journal of the Geological Society
- Vol. 141 (3), 581-591
- https://doi.org/10.1144/gsjgs.141.3.0581
Abstract
No abstract availableThis publication has 16 references indexed in Scilit:
- The character and evolution of hydrothermal fluids associated with the kaolinized St. Austell granite, SW EnglandJournal of the Geological Society, 1983
- The effect of fluorine on liquidus phase relationships in the system Qz-Ab-Or with excess water at 1 kbContributions to Mineralogy and Petrology, 1981
- Thermal Aureoles of Igneous Intrusions: Some Possible Indications of Hydrothermal Convective CoolingThe Journal of Geology, 1981
- The solubility of fluorite in hydrothermal solutions, an experimental studyGeochimica et Cosmochimica Acta, 1979
- Transport phenomena in hydrothermal systems; cooling plutonsAmerican Journal of Science, 1977
- Transport phenomena in hydrothermal systems; the nature of porosityAmerican Journal of Science, 1977
- Observations on the formation of kaolinite in the St. Austell granite, CornwallClay Minerals, 1976
- Chemical aspects of hydrothermal alteration with emphasis on hydrogen metasomatismEconomic Geology, 1964
- The Occurrence of Zinnwaldite in CornwallClay Minerals, 1960
- MAGMATIC DIFFERENTIATION AND ALTERATION IN THE ST. AUSTELL GRANITEQuarterly Journal of the Geological Society, 1958