Geochemical Studies of the Ginyu Reservoir in the Kirishima Geothermal Field
- Location
- Kirishima, Japan
- Conference
- Japan International Geothermal Symposium
- Year
- 1988
- Session
- Case Study (Japan)
- Language
- English
Full text
424KB, opens in a new tab
Abstract
This is the presentation of the result of geochemical study based on chemical and isotope data of discharge fluids and surface waters in the Kirishima geothermal area. Almost discharge waters from the wells drilled in the Kirishima geothermal area are characterized by the near-neutral pH Na-K-CI-SOI type .and these discharge fluids are provided from the water-dominated hydrothermal system. The Ginyu Fault reservoir fluids would be derived from meteoric water which precipitated to the Ginyu area and east of the Ginyu area before 1953.
Copyright 1988, Japan International Geothermal Symposium. 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.