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Seismic monitoring at the Geysers geothermal field, California

January 1, 1978

Two distinct clusters of microearthquakes have been identified at The Geysers, possibly relating to two independent pressure sinks resulting from steam production described by Lipman, and others (1977). Unlike earthquakes in the Maacama-Rodgers Creek fault zone to the south and west, earthquakes at The Geysers are confined to depths of less than 5 km. The present level of seismicity at The Geysers appears to be higher than the preproduction level and is higher and more continuous than the seismicity in the surrounding region. Earthquakes in the steam production zone at The Geysers resemble earthquakes in the surrounding region with regard to focal plane solutions, source characteristics and magnitude distribution (b slope). Subtle differences in earthquake characteristics may be resolved by analysis of more extensive data now being gathered in the region.

Publication Year 1978
Title Seismic monitoring at the Geysers geothermal field, California
DOI 10.3133/ofr78798
Authors S.M. Marks, R.S. Ludwin, K.B. Louie, C. G. Bufe
Publication Type Report
Publication Subtype USGS Numbered Series
Series Title Open-File Report
Series Number 78-798
Index ID ofr78798
Record Source USGS Publications Warehouse