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Sub-surface structures and site effects extracted from ambient noise in metropolitan Guangzhou, China
Abstract In this paper, ambient noise is used to investigate near-surface structures and site effects in metropolitan Guangzhou. We deployed 94 short period stations across Guangzhou area, and later a dense linear array across the Shougouling Fault (SF). Using more than one month's continuous data, we invert three-dimensional shear wave velocity structures of Guangzhou area via ambient noise tomography. Results show low velocity near the Guangzhou-Conghua Fault (GCF), Shougouling Fault (SF), and beneath the alluvial plain in the south region. Meanwhile, high-velocity anomalies are beneath the mountain area in northeastern region. Moreover, we obtain the sediment thickness and sub-surface shear wave velocity structures around the Shougouling Fault (SF) by horizontal to vertical spectral ratio (HVSR) method. HVSR results show a significant shift in the thickness of the sedimentary layer across the SF. Shear wave velocity derived from HVSR curves has a consistent trend of variation with the sediment thickness. Our results provide a better understanding of sub-surface structures of metropolitan Guangzhou, and can be served as a reference model for geological disaster migration prediction in the city.
Highlights Ambient noise tomography and HVSR method are applied to investigate subsurface structures and site effects in Guangzhou. Ambient noise tomography results show major faults across Guangzhou as low velocities, and mountain areas as high velocities. The site effect results reveal a low potential for ground damage near the Shougouling Fault (SF).
Sub-surface structures and site effects extracted from ambient noise in metropolitan Guangzhou, China
Abstract In this paper, ambient noise is used to investigate near-surface structures and site effects in metropolitan Guangzhou. We deployed 94 short period stations across Guangzhou area, and later a dense linear array across the Shougouling Fault (SF). Using more than one month's continuous data, we invert three-dimensional shear wave velocity structures of Guangzhou area via ambient noise tomography. Results show low velocity near the Guangzhou-Conghua Fault (GCF), Shougouling Fault (SF), and beneath the alluvial plain in the south region. Meanwhile, high-velocity anomalies are beneath the mountain area in northeastern region. Moreover, we obtain the sediment thickness and sub-surface shear wave velocity structures around the Shougouling Fault (SF) by horizontal to vertical spectral ratio (HVSR) method. HVSR results show a significant shift in the thickness of the sedimentary layer across the SF. Shear wave velocity derived from HVSR curves has a consistent trend of variation with the sediment thickness. Our results provide a better understanding of sub-surface structures of metropolitan Guangzhou, and can be served as a reference model for geological disaster migration prediction in the city.
Highlights Ambient noise tomography and HVSR method are applied to investigate subsurface structures and site effects in Guangzhou. Ambient noise tomography results show major faults across Guangzhou as low velocities, and mountain areas as high velocities. The site effect results reveal a low potential for ground damage near the Shougouling Fault (SF).
Sub-surface structures and site effects extracted from ambient noise in metropolitan Guangzhou, China
Wang, Shuang (author) / Sun, Xinlei (author) / Liu, Lanbo (author) / Zong, Jianye (author)
Engineering Geology ; 268
2020-02-13
Article (Journal)
Electronic Resource
English
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