The Pamir Frontal Thrust Fault: Holocene Full‐Segment Ruptures and Implications for Complex Segment Interactions in a Continental Collision Zone-Reference-Cited by-同舟云学术

The Pamir Frontal Thrust Fault: Holocene Full‐Segment Ruptures and Implications for Complex Segment Interactions in a Continental Collision Zone

Published:2021-12 Issue:12 Volume:126 Page:
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:JGR Solid Earth

Author:

Patyniak M.¹^ORCID,Landgraf A.²^ORCID,Dzhumabaeva A.³,Baikulov S.³,Williams A. M.⁴,Weiss J.R.¹^ORCID,Hilley G. E.⁵^ORCID,Preusser F.⁶^ORCID,Abdrakhmatov K. E.³^ORCID,Arrowsmith R. J⁴^ORCID,Strecker M. R.¹^ORCID

Affiliation:

1. Institute of Geoscience University of Potsdam Potsdam‐Golm Germany

2. NAGRA Wettingen Switzerland

3. Institute of Seismology National Academy of Science of Kyrgyzstan Bishkek Kyrgyzstan

4. School of Earth and Space Exploration Arizona State University Tempe AZ USA

5. Department of Geological Sciences Stanford University Stanford CA USA

6. Institute of Earth and Environmental Sciences University of Freiburg Freiburg Germany

Funder

Bundesministerium für Bildung und Forschung

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/10.1029/2021JB022405

Reference153 articles.

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3. Exhumational history of the north central Pamir

4. Earthquake size as a function of fault slip rate;Anderson J. G.;Bulletin of the Seismological Society of America,1996

5. The angular velocities of the plates and the velocity of Earth's centre from space geodesy

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