Transient scattering of elastic waves by dipping layers of arbitrary shape. Part 2: Plane strain model
- 1 April 1989
- journal article
- research article
- Published by Wiley in Earthquake Engineering & Structural Dynamics
- Vol. 18 (3) , 417-434
- https://doi.org/10.1002/eqe.4290180309
Abstract
No abstract availableKeywords
This publication has 7 references indexed in Scilit:
- Transient Scattering of Elastic Waves by Dipping Layers of Arbitrary Shape Part 1: Antiplane Strain ModelEarthquake Engineering & Structural Dynamics, 1989
- The two-dimensional resonance of sediment-filled valleysBulletin of the Seismological Society of America, 1985
- Surface motion of topographical irregularities for incidentP, SV,and Rayleigh wavesBulletin of the Seismological Society of America, 1985
- Observed variations of earthquake motion across a sediment-filled valleyBulletin of the Seismological Society of America, 1984
- The seismic response of sediment-filled valleys. Part 2. The case of incidentPandSVwavesBulletin of the Seismological Society of America, 1980
- Boundary methods: A criterion for completenessProceedings of the National Academy of Sciences, 1980
- Connectivity as an alternative to boundary integral equations: Construction of basesProceedings of the National Academy of Sciences, 1978