Possible Mechanisms for Generation of Anomalously High PGA During the 2011 Tohoku Earthquake
Author:
Funder
Russian Foundation for Basic Research
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
http://link.springer.com/article/10.1007/s00024-017-1558-2/fulltext.html
Reference44 articles.
1. Aagaard, B. T., & Heaton, T. H. (2004). Near-source ground motions from simulations of sustained intersonic and supersonic fault ruptures. Bulletin of the Seismological Society of America, 94, 2064–2078.
2. Archuleta, R. J. (1984). A faulting model for the 1979 Imperial Valley earthquake. Journal of Geophysical Research, 89, 4559–4585.
3. Asano, K., & Iwata, T. (2012). Source model for strong ground motion generation in the frequency range 01-10 Hz during the 2011 Tohoku earthquake. The Earth, Planets and Space, 64(12), 1111–1123.
4. Bonilla, L. F., Tsuda, K., Pulido, N., Regnier, J., & Laurendeau, A. (2011). Nonlinear site response evidence of K-NET and KiK-net records. The Earth, Planets and Space, 63, 785–789.
5. Bouchon, M., Bouin, M.-P., Karabulut, H., Toksoz, M. N., Dietrich, M., & Rosakis, A. J. (2001). How fast is rupture during an earthquake? New insights from the 1999 Turkey earthquakes. Geophysical Research Letters, 28, 2723–2726.
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