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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Published in | Acta seismologica sinica Vol. 18; no. 2; pp. 162 - 170 |
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Main Author | |
Format | Journal Article |
Language | Chinese 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 |
Subjects | |
Online Access | Get full text |
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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. |
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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 SourceType-Scholarly Journals-1 ObjectType-Feature-1 content type line 14 ObjectType-Article-1 ObjectType-Feature-2 content type line 23 ObjectType-Article-2 |
ISSN: | 1674-4519 1000-9116 1867-8777 1993-1344 |
DOI: | 10.1007/s11589-005-0063-3 |