Slip Rate Variation Along the Kunlun Fault (Tibet): Results From New GPS 
Observations and a Viscoelastic Earthquake‐Cycle Deformation Model

Diao, Faqi; Xiong, Xiong; Wang, R.; Walter, T. R.; Wang, Yuebing; Wang, Kai

doi:10.1029/2019GL081940

Item

ITEM ACTIONSEXPORT

Add to Basket

Local TagsRelease HistoryDetailsSummary

Released

Journal Article

Slip Rate Variation Along the Kunlun Fault (Tibet): Results From New GPS Observations and a Viscoelastic Earthquake‐Cycle Deformation Model

Authors

Diao, Faqi
External Organizations;

Xiong, Xiong
External Organizations;

/persons/resource/wang

Wang, R.
2.1 Physics of Earthquakes and Volcanoes, 2.0 Geophysics, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

/persons/resource/twalter

Walter, T. R.
2.1 Physics of Earthquakes and Volcanoes, 2.0 Geophysics, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

Wang, Yuebing
External Organizations;

Wang, Kai
External Organizations;

External Ressource

No external resources are shared

Fulltext (public)

4161912.pdf
(Publisher version), 5MB

Supplementary Material (public)

There is no public supplementary material available

Citation

Diao, F., Xiong, X., Wang, R., Walter, T. R., Wang, Y., Wang, K. (2019): Slip Rate Variation Along the Kunlun Fault (Tibet): Results From New GPS Observations and a Viscoelastic Earthquake‐Cycle Deformation Model. - Geophysical Research Letters, 46, 5, 2524-2533.
https://doi.org/10.1029/2019GL081940

Cite as: https://gfzpublic.gfz-potsdam.de/pubman/item/item_4161912

Abstract

There is no abstract available