Modelling the Alteration Halo of a Diorite Intrusion
- Conference
- New Zealand Geothermal Workshop
- Year
- 1998
- Session
- IEA - Deep Geothermal Resources
- Language
- English
Full text
586KB, opens in a new tab
Abstract
In this paper we first calculate the chemical and physical conditions in a geothermal reservoir containing Then we consider the effect of a pulse of magmatic vapour into the base of this reservoir and calculate the changed chemical and physical conditions as the reservoir is allowed to evolve for a further years. The chemistry in the reservoir is described by eleven componentspecies, HS', and Associated with these components are 32 secondary species and nine minerals.
Copyright 1998, 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.