Distribution of Lg coda Q in Xinjiang and its adjacent regions

In this study, we collected 1 156 broadband vertical components records at 22 digital seismic stations in Xinjiang region, Ueruemqi station, and 7 stations in the adjacent regions during the period of 1999-2003. The records were firstly processed by the stacked spectral ratio method to obtain Q sub(...

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Bibliographic Details
Published inActa seismologica sinica Vol. 18; no. 2; pp. 162 - 170
Main Author 徐彦 毛燕 胡家富 苏有锦 丛连理
Format Journal Article
LanguageChinese
English
Published Beijing Springer Nature B.V 01.03.2005
Department of Geophysics, Yunnan University, Kunming 650091, China
Earthquake Administration of Yunnan Province, Kunming 650041, China%Department of Geophysics, Yunnan University, Kunming 650091, China%Earthquake Administration of Yunnan Province, Kunming 650041, China
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Summary:In this study, we collected 1 156 broadband vertical components records at 22 digital seismic stations in Xinjiang region, Ueruemqi station, and 7 stations in the adjacent regions during the period of 1999-2003. The records were firstly processed by the stacked spectral ratio method to obtain Q sub(0) (Q at 1 Hz) and the frequency correlation factor corresponding to each path. Based on the results, the distribution images of Q sub(0) and in 11 grids for Xinjiang region were gained by the back-projection technique. The results indicate that Q sub(0) is high (300-450) in the Tarim platform and marginal Siberian platform, while Q sub(0) is low (150-250) in the southern regions as west Kunlun fold system and Songpan-Ganzi fold system. In the northern regions as Junggar fold system and Tianshan fold system, Q sub(0) is also low (250-300) and varies between 0.5 and 0.9.
Bibliography:11-5695/P
XU Yan MAO Yan1 HU Jia-fu1 SU You-jin2) CONG Lian-li1) 1) Department of Geophysics, Yunnan University, Kunming 650091, China 2) Earthquake Administration of Yunnan Province, Kunming 650041, China
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ISSN:1674-4519
1000-9116
1867-8777
1993-1344
DOI:10.1007/s11589-005-0063-3