Long-Delayed Aftershocks in New Zealand and the 2016 M7.8 Kaikoura Earthquake

Author:

Shebalin P.ORCID,Baranov S.

Funder

Russian Science Foundation

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Reference39 articles.

1. Aki, K. (1965). Maximum likelihood estimate of b in the formula log N = a − b M and its confidence limits. Bulletin of the Earthquake Research Institute, University of Tokyo, 43, 237–239.

2. Baranov, S. V., & Shebalin, P. N. (2016). Forecasting aftershock activity: 1. Adaptive estimates based on the Omori and Gutenberg–Richter laws. Izvestiya-Physics of the Solid Earth, 52(3), 413–431. doi: 10.1134/S1069351316020038 .

3. Baranov, S. V., & Shebalin, P. N. (2017). Forecasting aftershock activity: 2. Estimating the area prone to strong aftershocks. Izvestiya-Physics of the Solid Earth. doi: 10.7868/S0002333717020028 .

4. Bender, B. (1983). Maximum likelihood estimation of b-values for magnitude grouped data. Bulletin of the Seismological Society of America, 73, 831–851.

5. Cattania, C., Hainzl, S., Wang, L., Roth, F., & Enescu, B. (2014). Propagation of Coulomb stress uncertainties in physics-based aftershock models. Journal of Geophysical Research: Solid Earth, 119(10), 7846–7864.

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