Mapping deeply‐buried geothermal faults using microtremor array analysis

SUMMARY In this paper, the spatial autocorrelation microtremor array analysis is utilized to map deeply‐buried subtle faults that have primary controls on geothermal reservoirs. We identified a low‐velocity anomaly which is approximately 50 m wide at about 550–1400 m deep. A well drilled based on th...

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Veröffentlicht in:Geophysical journal international 2012-01, Vol.188 (1), p.115-122
Hauptverfasser: Xu, Peifen, Ling, Suqun, Li, Chuanjin, Du, Jianguo, Zhang, Dengming, Xu, Xueqiu, Dai, Kangming, Zhang, Zuohong
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container_end_page 122
container_issue 1
container_start_page 115
container_title Geophysical journal international
container_volume 188
creator Xu, Peifen
Ling, Suqun
Li, Chuanjin
Du, Jianguo
Zhang, Dengming
Xu, Xueqiu
Dai, Kangming
Zhang, Zuohong
description SUMMARY In this paper, the spatial autocorrelation microtremor array analysis is utilized to map deeply‐buried subtle faults that have primary controls on geothermal reservoirs. We identified a low‐velocity anomaly which is approximately 50 m wide at about 550–1400 m deep. A well drilled based on this anomaly later successfully produced hot water and further proved that the low‐velocity anomaly was caused by a highly fractured zone at depths from 700 to 1500 m. Our results clearly demonstrate that the microtremor survey method can be effectively utilized to map deeply‐buried faults and structures for geothermal energy exploration. The most effective way to increase the drilling success rate and, hence reduce the geothermal exploration risk, seems to be the development of new exploration methods and the integration of various geophysical technologies.
doi_str_mv 10.1111/j.1365-246X.2011.05266.x
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source Oxford Journals Open Access Collection; Wiley Online Library Journals Frontfile Complete
subjects Anomalies
Arrays
Asia
Drilling
Exploration
Faults
Fractures and faults
Geophysics
Geothermal
Hot water
Hydrogeophysics
Hydrothermal systems
Time series analysis
title Mapping deeply‐buried geothermal faults using microtremor array analysis
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