Interaction of geometry and mechanical property of trapezoidal sedimentary basins with incident SH waves

Author:

Zhu Chuanbin,Thambiratnam David

Publisher

Springer Science and Business Media LLC

Subject

Geophysics,Geotechnical Engineering and Engineering Geology,Building and Construction,Civil and Structural Engineering

Reference57 articles.

1. Adams BM, Neal MO, Taber JJ (2003) The basin-edge effect from weak ground motions across the fault-bounded edge of the Lower Hutt Valley, New Zealand. Bull Seismol Soc Am 93(6):2703–2716

2. Aki K, Larner KL (1970) Surface motion of a layered medium having an irregular interface due to incident plane SH waves. J Geophys Res 75:933–954

3. Aki K, Richards PG (1980) Quantitative seismology: theory and methods, vols I, II. WH. Freeman and Company, New York

4. Alterman Z, Karal FC (1968) Propagation of elastic waves in layered media by finite difference methods. Bull Seismol Soc Am 63:615–632

5. Bard PY, Bouchon M (1980a) The seismic response of sediment-filled valleys. Part 1. The case of incident SH waves. Bull Seismol Soc Am 70(4):1263–1286

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