The 2017 Mw 7.3 Ezgeleh, Iran earthquake determined from InSAR measurements and teleseismic waveforms

Author:

Ding Kaihua1ORCID,He Ping2,Wen Yangmao3,Chen Yunguo2,Wang Dun4,Li Shuiping2,Wang Qi2

Affiliation:

1. Faculty of Information Engineering, China University of Geosciences, Wuhan 430074, China

2. Institute of Geophysics and Geomatics, China University of Geosciences, Wuhan 430074, China

3. School of Geodesy and Geomatics, Wuhan University, Wuhan 430079, China

4. School of Earth Sciences, China University of Geosciences, Wuhan 430074, China

Funder

National Natural Science Foundation of China

China Postdoctoral Science Foundation

Fundamental Research Funds for National Universities

Hubei Subsurface Multi-scale Imaging Key Laboratory

China University of Geosciences, Wuhan, and Key Laboratory of Geospace Environment and Geodesy, Ministry of Education, Wuhan University

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

Reference34 articles.

1. Magnitude calibration of north Indian earthquakes;Ambraseys;Geophys. J. Int.,2004

2. Lower edge of locked Main Himalayan Thrust unzipped by the 2015 Gorkha earthquake;Avouac;Nat. Geosci.,2015

3. Patterns of historical earthquake rupture in the Iranian plateau;Berberian;Bull. seism. Soc. Am.,1999

4. Phase unwrapping for large SAR interferograms: statistical segmentation and generalized network models;Chen;IEEE Trans. Geosci. Remote Sens.,2002

5. Geodetic investigation of the 13 May 1995 Kozani-Grevena (Greece) Earthquake;Clarke;Geophys. Res. Lett.,1997

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