Temporal changes of seismicity in Salton Sea Geothermal Field due to distant earthquakes and geothermal productions
The Salton Sea Geothermal Field (SSGF) is one of the most seismically active and geothermally productive fields in California. Here we present a detailed analysis of short-term seismicity change in SSGF from 2008 to 2013 during and right following large distant earthquakes, as well as long-term seis...
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sg-ntu-dr.10356-1703842023-09-12T15:36:29Z Temporal changes of seismicity in Salton Sea Geothermal Field due to distant earthquakes and geothermal productions Li, Chenyu Peng, Zhigang Yao, Dongdong Meng, Xiaofeng Zhai, Qiushi Earth Observatory of Singapore Science::Geology Induced Seismicity Salton Sea Geothermal Field The Salton Sea Geothermal Field (SSGF) is one of the most seismically active and geothermally productive fields in California. Here we present a detailed analysis of short-term seismicity change in SSGF from 2008 to 2013 during and right following large distant earthquakes, as well as long-term seismicity change due to geothermal productions. We first apply a GPU-based waveform matched-filter technique (WMFT) to the continuous data recorded by the Calenergy Borehole (EN) Network and detect more than 70 000 new micro-earthquakes than listed in the standard Southern California Seismic Network catalogue. We then analyse the seismicity rate changes in the SSGF associated with transient stress fluctuations triggered by regional and large teleseismic earthquakes from 1999 to 2019. We find triggered seismicity in the SSGF following seven regional M > 5.5 earthquakes. In comparison, most teleseismic earthquakes with M > 8.0 did not trigger significant seismicity rate change in the SSGF, likely indicating a frequency dependence in remote dynamic triggering. We further characterize the correlation between the long-term seismicity rate and geothermal production rates, and the temporal and spatial distribution of Guttenberg-Richter b-values inside and outside the SSGF with the newly detected catalogue. The long-term seismicity shows that events with M > 1.5 are likely correlated with net production rates, while smaller events do not show any correlation. The b-values inside the SSGF are higher than those outside the SSGF, and the locations of dynamically triggered events are close to locations with high b-values. Published version This research was supported by the Southern California Earthquake Center (contribution no. 11964, award nos 10010 and 17230). SCEC is funded by NSF Cooperative Agreement EAR-1600087 and USGS Cooperative Agreement G17AC00047. 2023-09-11T02:53:30Z 2023-09-11T02:53:30Z 2023 Journal Article Li, C., Peng, Z., Yao, D., Meng, X. & Zhai, Q. (2023). Temporal changes of seismicity in Salton Sea Geothermal Field due to distant earthquakes and geothermal productions. Geophysical Journal International, 232(1), 287-299. https://dx.doi.org/10.1093/gji/ggac324 0956-540X https://hdl.handle.net/10356/170384 10.1093/gji/ggac324 2-s2.0-85144418521 1 232 287 299 en Geophysical Journal International This article has been accepted for publication in Geophysical Journal International. © 2022 The Author(s). Published by Oxford University Press on behalf of The Royal Astronomical Society. All rights reserved. application/pdf |
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Science::Geology Induced Seismicity Salton Sea Geothermal Field Li, Chenyu Peng, Zhigang Yao, Dongdong Meng, Xiaofeng Zhai, Qiushi Temporal changes of seismicity in Salton Sea Geothermal Field due to distant earthquakes and geothermal productions |
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The Salton Sea Geothermal Field (SSGF) is one of the most seismically active and geothermally productive fields in California. Here we present a detailed analysis of short-term seismicity change in SSGF from 2008 to 2013 during and right following large distant earthquakes, as well as long-term seismicity change due to geothermal productions. We first apply a GPU-based waveform matched-filter technique (WMFT) to the continuous data recorded by the Calenergy Borehole (EN) Network and detect more than 70 000 new micro-earthquakes than listed in the standard Southern California Seismic Network catalogue. We then analyse the seismicity rate changes in the SSGF associated with transient stress fluctuations triggered by regional and large teleseismic earthquakes from 1999 to 2019. We find triggered seismicity in the SSGF following seven regional M > 5.5 earthquakes. In comparison, most teleseismic earthquakes with M > 8.0 did not trigger significant seismicity rate change in the SSGF, likely indicating a frequency dependence in remote dynamic triggering. We further characterize the correlation between the long-term seismicity rate and geothermal production rates, and the temporal and spatial distribution of Guttenberg-Richter b-values inside and outside the SSGF with the newly detected catalogue. The long-term seismicity shows that events with M > 1.5 are likely correlated with net production rates, while smaller events do not show any correlation. The b-values inside the SSGF are higher than those outside the SSGF, and the locations of dynamically triggered events are close to locations with high b-values. |
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Earth Observatory of Singapore |
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Earth Observatory of Singapore Li, Chenyu Peng, Zhigang Yao, Dongdong Meng, Xiaofeng Zhai, Qiushi |
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Article |
author |
Li, Chenyu Peng, Zhigang Yao, Dongdong Meng, Xiaofeng Zhai, Qiushi |
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Li, Chenyu |
title |
Temporal changes of seismicity in Salton Sea Geothermal Field due to distant earthquakes and geothermal productions |
title_short |
Temporal changes of seismicity in Salton Sea Geothermal Field due to distant earthquakes and geothermal productions |
title_full |
Temporal changes of seismicity in Salton Sea Geothermal Field due to distant earthquakes and geothermal productions |
title_fullStr |
Temporal changes of seismicity in Salton Sea Geothermal Field due to distant earthquakes and geothermal productions |
title_full_unstemmed |
Temporal changes of seismicity in Salton Sea Geothermal Field due to distant earthquakes and geothermal productions |
title_sort |
temporal changes of seismicity in salton sea geothermal field due to distant earthquakes and geothermal productions |
publishDate |
2023 |
url |
https://hdl.handle.net/10356/170384 |
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1779156262625214464 |