Pre- and Post-seismic Crustal Stress Heterogeneity Analogous to 14 November 2016, Mw 7.8, Kaikoura Earthquake, New Zealand
Author:
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
https://link.springer.com/content/pdf/10.1007/s00024-023-03308-9.pdf
Reference53 articles.
1. Aki, K. (1965). Maximum likelihood estimate of b in the formula log N = a–bM and its confidence limits. Bulletin of the Earthquake Research Institute, 43, 237–239.
2. Amitrano, D. (2003). Brittle-ductile transition and associated seismicity: Experimental and numerical studies and relationship with the b value. Journal of Geophysical Research: Solid Earth. https://doi.org/10.1029/2001jb000680
3. Angelier, J. (1979). Determination of the mean principal directions of stresses for a given fault population. Tectonophysics, 56, T17–T26. https://doi.org/10.1016/0040-1951(79)90081-7
4. Beavan, J., Tregoning, P., Bevis, M., Kato, T., & Meertens, C. (2002). Motion and rigidity of the Pacific Plate and implications for plate boundary deformation. Journal of Geophysical Research: Solid Earth, 107(B10), ETG 19-1-ETG 19–15. https://doi.org/10.1029/2001JB000282
5. Chamberlain, C. J., Frank, W. B., Lanza, F., Townend, J., & Warren-Smith, E. (2021). Illuminating the pre-, co-, and post-seismic phases of the 2016 M7.8 Kaikōura earthquake with 10 years of seismicity. Journal of Geophysical Research: Solid Earth. https://doi.org/10.1029/2021JB022304
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