Relationship Between Seismic Moment and Source Duration for Seismogenic Earthquakes in Taiwan: Implications for the Product of Static Stress Drop and the Cube of Rupture Velocity
Author:
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
http://link.springer.com/content/pdf/10.1007/s00024-020-02429-9.pdf
Reference78 articles.
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2. Allmann, B. P., & Shearer, P. M. (2009). Global variations of stress drop for moderate to large earthquakes. Journal Geophysical Research,114, B01310. https://doi.org/10.1029/2008JB005821.
3. Causse, M., & Song, S. G. (2015). Are stress drop and rupture velocity of earthquakes independent? Insight from observed ground motion variability. Geophysical Research Letters,42, 7383–7389.
4. Chao, W. A., Zhao, L., Wu, Y. M., & Lee, S. J. (2013). Imaging source slip distribution by the back-projection of P-wave amplitudes from strong-motion records: A case study for the 2010 Jiasian, Taiwan, earthquake. Geophysical Journal International,193, 1713–1725.
5. Chen, K. C., Huang, W. G., & Wang, J. H. (2007). Relationships among magnitudes and seismic moment of earthquakes in the Taiwan region. Terrestrial, Atmospheric and Oceanic Sciences,18, 951–973.
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