Dispersion attenuation structure of the crust around the Weifang-Jiashan segment of the Tanlu fault zone in North China

Author:

Liu Xiqiang,Li Qinghe,Li Hong

Publisher

Earthquake Science

Subject

Geology,Geophysics,Geotechnical Engineering and Engineering Geology

Reference29 articles.

1. Chao H T, Li J L, Cui Z W and Zhao Q Y (1997). Mode of motion of the holocene fault in Weifang-Jiashan segment of the Tanlu fault zone and earthquake generating model. J Seism Res20(2): 218–226 (in Chinese with English abstract).

2. Chao H T, Li J L, Cui Z W, Man H M and Du X S (1995). Active faults in Tanlu (Tancheng-Lujiang) Fault Zone and the hazards produced by the 1668 Tancheng earthquake (M=8.5). Marine Geology and Quaternary Geology15(3): 69–80 (in Chinese with English abstract).

3. Cong L, Mejia J and Mitchell B J (2000). Attenuation dispersion of P waves in and near the New Madrid seismic zone. Bull Seismol Soc Am90(3): 679–689.

4. Correig A M and Mitchell B J (1989). Attenuative dispersion at La Cerdanya, eastern Pyrenees. Phys Earth Planet Inter57: 304–310.

5. Feng D Y (1981). Seismic Wave Velocity Anomaly. Seismological Press, Beijing, 21–33 (in Chinese).

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