Dynamic Source Model for the 2011 Tohoku Earthquake in a Wide Period Range Combining Slip Reactivation with the Short-Period Ground Motion Generation Process-Reference-Cited by-同舟云学术

Dynamic Source Model for the 2011 Tohoku Earthquake in a Wide Period Range Combining Slip Reactivation with the Short-Period Ground Motion Generation Process

Published:2019-05-17 Issue:5 Volume:177 Page:2143-2161
ISSN:0033-4553
Container-title:Pure and Applied Geophysics
language:en
Short-container-title:Pure Appl. Geophys.

Author:

Galvez Percy,Petukhin Anatoly^ORCID,Irikura Kojiro,Somerville Paul

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/s00024-019-02210-7.pdf

Reference66 articles.

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2. Avouac, J.-P., Meng, L., Wei, S., Wang, T., & Ampuero, J. P. (2015). Lower edge of locked main Himalayan thrust unzipped by the 2015 Gorkha earthquake. Nature Geoscience,8, 708–711. https://doi.org/10.1038/ngeo2518 .

3. Beroza, G. C., & Mikumo, T. (1996). Short slip duration in dynamic rupture in the presence of heterogeneous fault properties. Journal of Geophysical Research,101, 22449.

4. Bouchon, M. (1981). A simple method to calculate Green’s function for elastic layered media. Bulletin of the Seismological Society of America,71, 959.

5. Chen, X., Madden, A., & Reches, Z. (2017). Friction evolution of granitic faults: Heating controlled transition from powder lubrication to frictional melt. Journal of Geophysical Research,122, 9275.

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