Measurements of Post-seismic Stress State to 700 Meters Depth Using Anelastic Strain Recovery Method in Source Area of the 2016 Kumamoto Earthquakes
Author:
Affiliation:
1. Graduate School of Engineering, Kyoto University
Publisher
Japan Society of Engineering Geology
Link
https://www.jstage.jst.go.jp/article/jjseg/62/1/62_13/_pdf
Reference35 articles.
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3. 3)Hardebeck, J. L.(2012): Coseismic and postseismic stress rotations due to great subduction zone earthquakes, Geophys. Res. Lett., Vol. 39, L21313, https://doi.org/10.1029/2012GL053438.
4. 4)Toda, S., Stein, R. S., Reasenberg, P. A., Dieterich, J. H., and Yoshida, A.(1998): Stress transferred by the 1995 Mw = 6.9 Kobe, Japan, shock: Effect on aftershocks and future earthquake probabilities, J. Geophys. Res. Solid Earth., Vol. 103, No. B10, pp. 24,543-24,565, https://doi.org/10.1029/98JB00765.
5. 5)Stein, R. S.(1999): The role of stress transfer in earthquake occurrence, Nature, Vol. 402, pp. 605-609, https://doi.org/10.1038/45144.
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