Probing the Upper End of Intracontinental Earthquake Magnitude: A Prehistoric Example From the Dzhungarian and Lepsy Faults of Kazakhstan-Reference-Cited by-同舟云学术

Probing the Upper End of Intracontinental Earthquake Magnitude: A Prehistoric Example From the Dzhungarian and Lepsy Faults of Kazakhstan

Published:2022-10 Issue:10 Volume:41 Page:
ISSN:0278-7407
Container-title:Tectonics
language:en
Short-container-title:Tectonics

Author:

Tsai C.‐H.¹^ORCID,Abdrakhmatov K.²,Mukambayev A.³,Elliott A. J.⁴^ORCID,Elliott J. R.⁵^ORCID,Grützner C.⁶,Rhodes E. J.⁷^ORCID,Ivester A. H.⁷,Walker R. T.¹,Wilkinson R.¹^ORCID

Affiliation:

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

2. Kyrgyz Institute of Seismology Bishkek Kyrgyzstan

3. Kazakhstan National Data Center Satbayev University Almaty Kazakhstan

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

5. COMET, School of Earth and Environment University of Leeds Leeds UK

6. Institute of Geological Sciences Friedrich Schiller University Jena Jena Germany

7. Department of Geography University of Sheffield Sheffield UK

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2022TC007300

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4. Origin, direction, and rate of modern compression of the central Tien Shan (Kyrgyzstan);Abdrakhmatov K. E.;Russian Geology and Geophysics,2001

5. Variability in surface rupture between successive earthquakes on the Suusamyr Fault, Kyrgyz Tien Shan: implications for palaeoseismology

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