Intrinsic and attenuative dispersion characteristics of direct P-waves in and near the source area of the 1999 MW7.6 Chi-Chi, Taiwan, earth- quake before and after the mainshock
Author:
Publisher
Earthquake Science
Subject
Geology,Geophysics,Geotechnical Engineering and Engineering Geology
Link
http://link.springer.com/content/pdf/10.1007/s11589-009-0033-2
Reference44 articles.
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2. Al-Shukri H J and Mitchell B J (1988). Reduced seismic velocities in the source zone of New Madrid earthquakes. Bull Seism Soc Amer78:1 491–1 509.
3. Akbar N, Dvorkin J and Nur A (1993). Relating P- wave attenuation to permeability. Geophysics58(1): 20–29.
4. Aytug H and Saydam C (2002). Solving large-scale maximum expected covering location problems by genetic algorithms: A comparative study. European Journal of Operational Research141: 480–494.
5. Castro R R, Rebollar C J, Inzunza L, Orozco L, Sanchez J, Galvez O, Farfan F J and Mendez I (2003). Direct body-wave Q estimates in northern Baja California Mexico. Phys Earth Planet Interi103: 33–38.
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1. The seismogenic deformation and Qp temporal variation before the M6.2 Mingjen earthquake, Taiwan;Journal of Asian Earth Sciences;2015-12
2. Dispersion attenuation structure of the crust around the Weifang-Jiashan segment of the Tanlu fault zone in North China;Earthquake Science;2012-02
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