Possible Site Effects Revealed by Regional Earthquake Records in the Qaidam Basin, China
2018; Seismological Society of America; Volume: 90; Issue: 1 Linguagem: Inglês
10.1785/0220180095
ISSN1938-2057
Autores Tópico(s)Seismic Waves and Analysis
ResumoResearch Article| November 14, 2018 Possible Site Effects Revealed by Regional Earthquake Records in the Qaidam Basin, China Yanyang Chen; Yanyang Chen aDepartment of Geophysics, School of Earth and Space Sciences, Peking University, No. 5 Yiheyuan Road, Haidian District, Beijing 100871, China, ybwang@pku.edu.cn Search for other works by this author on: GSW Google Scholar Yanbin Wang Yanbin Wang aDepartment of Geophysics, School of Earth and Space Sciences, Peking University, No. 5 Yiheyuan Road, Haidian District, Beijing 100871, China, ybwang@pku.edu.cn Search for other works by this author on: GSW Google Scholar Seismological Research Letters (2019) 90 (1): 280–293. https://doi.org/10.1785/0220180095 Article history first online: 14 Nov 2018 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Yanyang Chen, Yanbin Wang; Possible Site Effects Revealed by Regional Earthquake Records in the Qaidam Basin, China. Seismological Research Letters 2018;; 90 (1): 280–293. doi: https://doi.org/10.1785/0220180095 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietySeismological Research Letters Search Advanced Search ABSTRACT Qaidam basin is the largest intermountain basin in northeastern Tibetan plateau. Broadband seismograms from 25 regional earthquakes with magnitudes greater than 4.0 were recorded by the International Deep Profiling of Tibet and the Himalaya Phase IV (INDEPTH IV) temporary seismic array as well as several permanent stations around the basin, allowing for the first investigation of site effects and ground‐motion amplification in the Qaidam basin. The seismograms are analyzed in both time and frequency domains. In the time domain, waveforms were amplified and of prolonged duration due to long‐period surface waves generated at the basin edges. Peak ground velocity (PGV) value within the basin is about 1~2 times of that predicted by attenuation relation. Response spectrum and two spectral ratio techniques are used in the frequency domain. Response spectra show obvious amplifications at longer periods within the basin. Horizontal‐to‐vertical spectral ratio (HVSR) does not significantly depend on the source back azimuths and magnitudes. HVSRs at stations located inside the basin have lower resonance frequencies and higher amplification factors than those located outside the basin, indicating that sediments in the basin have significant effect on the ground motion. Comparing HVSR with standard spectral ratio (SSR) at stations within the basin shows that both methods yield similar estimates for the resonance frequency, but the amplification factors estimated by SSR are much larger than that by HVSR, which suggests that HVSR may underestimate the amplification in the Qaidam basin. 2D seismic‐wave propagation modeling suggests that edge‐generated surface waves contribute to site amplification, especially for stations close to the basin boundary. Comparing the observed site amplification with prediction from Next Generation Attenuation‐West2 Project (NGA‐West2) ground‐motion prediction equation (GMPE) indicates that the prediction overestimates the amplification, and it is important to develop the GMPE for this region with increasing data and considering the appropriate site term. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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