Lower edge of locked Main Himalayan Thrust unzipped by the 2015 Gorkha earthquake-Reference-Cited by-同舟云学术

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Lower edge of locked Main Himalayan Thrust unzipped by the 2015 Gorkha earthquake

Published:2015-08-06 Issue:9 Volume:8 Page:708-711
ISSN:1752-0894
Container-title:Nature Geoscience
language:en
Short-container-title:Nature Geosci

Author:

Avouac Jean-Philippe,Meng Lingsen,Wei Shengji,Wang Teng,Ampuero Jean-Paul

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Link

http://www.nature.com/articles/ngeo2518.pdf

Reference42 articles.

1. Schurr, B. et al. Gradual unlocking of plate boundary controlled initiation of the 2014 Iquique earthquake. Nature 512, 299–302 (2014).

2. Loveless, J. P. & Meade, B. J. Spatial correlation of interseismic coupling and coseismic rupture extent of the 2011 Mw = 9.0 Tohoku-oki earthquake. Geophys. Res. Lett. 38, L17306 (2011).

3. Yue, H. et al. The 5 September 2012 Nicoya, Costa Rica Mw 7.6 earthquake rupture process from joint inversion of high-rate GPS, strong-motion, and teleseismic P wave data and its relationship to adjacent plate boundary interface properties. J. Geophys. Res. 118, 5453–5466 (2013).

4. Kaneko, Y., Avouac, J. P. & Lapusta, N. Towards inferring earthquake patterns from geodetic observations of interseismic coupling. Nature Geosci. 3, 363–369 (2010).

5. Ader, T. et al. Convergence rate across the Nepal Himalaya and interseismic coupling on the Main Himalayan Thrust: Implications for seismic hazard. J. Geophys. Res. 117, B04403 (2012).

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