Geothermal Reservoir Interpretation from Change in Gravity
- Location
- Taupo Volcanic Zone; Wairakei, New Zealand; The Geysers, California
- Conference
- Stanford Geothermal Workshop
- Year
- 1977
- Session
- Reservoir Physics
- Language
- English
Full text
402KB, opens in a new tab
Abstract
Precision gravity methods provide new information regarding geothermal reservoir mechanisms and depletion. This paper discusses the principles of present interpretations and early conclusions from two producing geothermal fields, Wairakei, in New Zealand, and The Geysers, California.
Copyright 1977, Stanford Geothermal Program. 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.