Imaging Shallow Velocity Structure of an Inactive Fault by Airgun Seismic Source: A Case Study of Xiliushui Fault in Qiliang Mountain

We observed high-quality waves from a repeatable airgun seismic source recorded by a linear ultra-dense seismic array across the Xiliushui fault zone, one of the inactive faults in the Qilian Mountain, on the northeastern margin of the Tibetan Plateau, China. We used Snell’s law of seismic ray propa...

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Main Authors: Manzhong Qin, Baichen Wu, Yi Wang, Xueyi Shang, Yuansheng Zhang, Xuzhou Liu, Xiao Guo, Rui Zou, Yahong Wang, Dianfeng Sun
Format: Article
Language:English
Published: MDPI AG 2025-01-01
Series:Geosciences
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Online Access:https://www.mdpi.com/2076-3263/15/1/16
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author Manzhong Qin
Baichen Wu
Yi Wang
Xueyi Shang
Yuansheng Zhang
Xuzhou Liu
Xiao Guo
Rui Zou
Yahong Wang
Dianfeng Sun
author_facet Manzhong Qin
Baichen Wu
Yi Wang
Xueyi Shang
Yuansheng Zhang
Xuzhou Liu
Xiao Guo
Rui Zou
Yahong Wang
Dianfeng Sun
author_sort Manzhong Qin
collection DOAJ
description We observed high-quality waves from a repeatable airgun seismic source recorded by a linear ultra-dense seismic array across the Xiliushui fault zone, one of the inactive faults in the Qilian Mountain, on the northeastern margin of the Tibetan Plateau, China. We used Snell’s law of seismic ray propagation to determine a simplified ambient velocity model. Based on the flexible and precise spectral element method, we computed broadband synthetic seismograms for a shallow low-velocity fault zone (FZ) to model the direct P-wave travel time delay and incident angle of the wavefield near the FZ. The FZ extent range and boundaries were inverted by apparent travel time delays and amplification patterns across the fault. According to prior information on the properties of the direct P-waves, we could constrain the inverse modeling and conduct a grid search for the fault parameters. The velocity reduction between the FZ and host rock, along with the dip angle of the FZ, were also constrained by the P-wave travel time delay systematic analysis and incoming angle of the P-waves. We found that the Xiliushui fault has a 70~80 m-wide low-velocity fault damage zone in which the P-wave velocity is reduced to ~40% with respect to the host rock. The fault damage zone dips ~35°southwest and extends to ~165 m in depth. The repeatability and environment protection characteristics of the airgun seismic survey and the economic benefits of a limited number of instruments setting are prominent.
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spelling doaj-art-53e630727bb2420f90c8566af9f8702c2025-01-24T13:34:10ZengMDPI AGGeosciences2076-32632025-01-011511610.3390/geosciences15010016Imaging Shallow Velocity Structure of an Inactive Fault by Airgun Seismic Source: A Case Study of Xiliushui Fault in Qiliang MountainManzhong Qin0Baichen Wu1Yi Wang2Xueyi Shang3Yuansheng Zhang4Xuzhou Liu5Xiao Guo6Rui Zou7Yahong Wang8Dianfeng Sun9Lanzhou Institute of Seismology, China Earthquake Administration, Lanzhou 730000, ChinaInstitute of Earthquake Forecasting, China Earthquake Administration, Beijing 100036, ChinaInstitute of Earthquake Forecasting, China Earthquake Administration, Beijing 100036, ChinaSchool of Resources and Safety Engineering, Chongqing University, Chongqing 400044, ChinaLanzhou Institute of Seismology, China Earthquake Administration, Lanzhou 730000, ChinaLanzhou Institute of Seismology, China Earthquake Administration, Lanzhou 730000, ChinaLanzhou Institute of Seismology, China Earthquake Administration, Lanzhou 730000, ChinaLanzhou Institute of Seismology, China Earthquake Administration, Lanzhou 730000, ChinaLanzhou Institute of Seismology, China Earthquake Administration, Lanzhou 730000, ChinaLanzhou Institute of Seismology, China Earthquake Administration, Lanzhou 730000, ChinaWe observed high-quality waves from a repeatable airgun seismic source recorded by a linear ultra-dense seismic array across the Xiliushui fault zone, one of the inactive faults in the Qilian Mountain, on the northeastern margin of the Tibetan Plateau, China. We used Snell’s law of seismic ray propagation to determine a simplified ambient velocity model. Based on the flexible and precise spectral element method, we computed broadband synthetic seismograms for a shallow low-velocity fault zone (FZ) to model the direct P-wave travel time delay and incident angle of the wavefield near the FZ. The FZ extent range and boundaries were inverted by apparent travel time delays and amplification patterns across the fault. According to prior information on the properties of the direct P-waves, we could constrain the inverse modeling and conduct a grid search for the fault parameters. The velocity reduction between the FZ and host rock, along with the dip angle of the FZ, were also constrained by the P-wave travel time delay systematic analysis and incoming angle of the P-waves. We found that the Xiliushui fault has a 70~80 m-wide low-velocity fault damage zone in which the P-wave velocity is reduced to ~40% with respect to the host rock. The fault damage zone dips ~35°southwest and extends to ~165 m in depth. The repeatability and environment protection characteristics of the airgun seismic survey and the economic benefits of a limited number of instruments setting are prominent.https://www.mdpi.com/2076-3263/15/1/16the fault zone seismic phaseairgun seismic sourcefault zone imagingbody waves modelingtravel time inversion
spellingShingle Manzhong Qin
Baichen Wu
Yi Wang
Xueyi Shang
Yuansheng Zhang
Xuzhou Liu
Xiao Guo
Rui Zou
Yahong Wang
Dianfeng Sun
Imaging Shallow Velocity Structure of an Inactive Fault by Airgun Seismic Source: A Case Study of Xiliushui Fault in Qiliang Mountain
Geosciences
the fault zone seismic phase
airgun seismic source
fault zone imaging
body waves modeling
travel time inversion
title Imaging Shallow Velocity Structure of an Inactive Fault by Airgun Seismic Source: A Case Study of Xiliushui Fault in Qiliang Mountain
title_full Imaging Shallow Velocity Structure of an Inactive Fault by Airgun Seismic Source: A Case Study of Xiliushui Fault in Qiliang Mountain
title_fullStr Imaging Shallow Velocity Structure of an Inactive Fault by Airgun Seismic Source: A Case Study of Xiliushui Fault in Qiliang Mountain
title_full_unstemmed Imaging Shallow Velocity Structure of an Inactive Fault by Airgun Seismic Source: A Case Study of Xiliushui Fault in Qiliang Mountain
title_short Imaging Shallow Velocity Structure of an Inactive Fault by Airgun Seismic Source: A Case Study of Xiliushui Fault in Qiliang Mountain
title_sort imaging shallow velocity structure of an inactive fault by airgun seismic source a case study of xiliushui fault in qiliang mountain
topic the fault zone seismic phase
airgun seismic source
fault zone imaging
body waves modeling
travel time inversion
url https://www.mdpi.com/2076-3263/15/1/16
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