Sediment Structures Constrained by Converted Waves From Local Earthquakes Recorded by a Dense Seismic Array in the Tangshan Earthquake Region
Author:
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
http://link.springer.com/content/pdf/10.1007/s00024-021-02667-5.pdf
Reference61 articles.
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2. Arai, H., & Tokimatsu, K. (2004). S-Wave Velocity Profiling by Inversion of Microtremor H/V Spectrum. Bulletin of the Seismological Society of America, 94(1), 53–63.
3. Bao, F., Li, Z., Tian, B., Wang, L., & Tu, G. (2019). Sediment thickness variations of the Tangshan fault zone in North China from a dense seismic array and microtremor survey. Journal of Asian Earth Sciences, in press.
4. Bao, F., Li, Z., Yuen, D., Zhao, J., Ren, J., & Tian, B. (2018). Shallow structure of the Tangshan fault zone unveiled by dense seismic array and horizontal-to-vertical spectral ratio method. Physics of the Earth and Planetary Interiors, 281, 46–54.
5. Bell, S. W., Ruan, Y., & Forsyth, D. W. (2015). Shear velocity structure of Abyssal Plain sediments in Cascadia. Seismological Research Letters, 86(5), 1247–1252.
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