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MONITORING OF A GEOTHERMAL RESERVOIR UTILIZING MICROEARTHQUAKES

Toshiyuki Tosha, Nobuo Doi, and Kazuo Koide

Key words
Microearthquake
Location
Kakkonda, Japan
Conference
Stanford Geothermal Workshop
Year
2000
Session
Geophysics
Language
English

Full text

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Abstract

Microearthquake observation was conducted in a geothermal field and hypocenters were determined by the seismic network data, revealing the extent of the geothermal reservoir. Compared with hypocenter distributions in the past, the region of high seismic activity had migrated. This temporal change is due to variations in the amount of re-injection fluid and the elongation of the fracture zone. Microearthquake observation is one of the more practical ways to monitor reservoirs in a geothermal field.

Copyright 2000, 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.

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