Equilibria Among Variable-Composition Minerals and Aqueous Solutions Under Hydrothermal Conditions
- Conference
- New Zealand Geothermal Workshop
- Year
- 1983
- Language
- English
Full text
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Abstract
Equilibrium phase relations stoichiometric mineral assemblages and are usually interpreted using logarithmic activity diagrams. utility because many of the found in nature contain minerals with highly variable composition. Using a model which considers ideal mixing of on completely or nearly homological sites in silicate examples of modified activity diagrams constructed for phase clay., epidote and chlorite. The method has
Copyright 1983, University of Auckland. Readers who download papers from this site should honour the copyright of the original authors, and may not copy or distribute the work further without the permission of the original publisher.