Magnitude of the 1920 Haiyuan Earthquake Reestimated Using Seismological and Geomorphological Methods-Reference-Cited by-同舟云学术

Magnitude of the 1920 Haiyuan Earthquake Reestimated Using Seismological and Geomorphological Methods

Published:2020-08 Issue:8 Volume:125 Page:
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:JGR Solid Earth

Author:

Ou Q.¹^ORCID,Kulikova G.²^ORCID,Yu J.¹³^ORCID,Elliott A.¹⁴^ORCID,Parsons B.¹,Walker R.¹^ORCID

Affiliation:

1. COMET, Department of Earth Sciences University of Oxford Oxford UK

2. Institute of Geosciences University of Potsdam Potsdam Germany

3. State Key Laboratory of Earthquake Dynamics Institute of Geology, China Earthquake Administration Beijing China

4. Now at the U.S. Geological Survey Earthquake Science Center Moffett Field CA USA

Funder

Natural Environment Research Council

Ministry of Science and Technology of the People's Republic of China

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019JB019244

Reference121 articles.

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3. Generation and propagation of G waves from the Niigata earthquake of June 16, 1964.: Part 2. Estimation of earthquake moment, released energy, and stress‐strain drop from the G wave spectrum;Aki K.;Bulletin of the Earthquake Research Institute, University of Tokyo,1966

4. Characterization of barriers on an earthquake fault

5. Bormann P.(2012).Magnitude calibration formulas and tables comments on their use and complementary data. (Vol. 1. Tech. Rep.) https://doi.org/10.2312/GFZ.NMSOP-2

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