Temporal changes in rock uplift rates of folds in the foreland of the Tian Shan and the Pamir from geodetic and geologic data-Reference-Cited by-同舟云学术

Temporal changes in rock uplift rates of folds in the foreland of the Tian Shan and the Pamir from geodetic and geologic data

Published:2017-11-14 Issue:21 Volume:44 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Bufe Aaron¹²³^ORCID,Bekaert David P. S.⁴^ORCID,Hussain Ekbal⁵^ORCID,Bookhagen Bodo²⁶^ORCID,Burbank Douglas W.¹²^ORCID,Thompson Jobe Jessica A.²⁷^ORCID,Chen Jie⁸,Li Tao⁸⁹,Liu Langtao⁸¹⁰,Gan Weijun⁸

Affiliation:

1. Department of Earth Sciences University of California Santa Barbara California USA

2. Earth Research Institute University of California Santa Barbara California USA

3. Now at GFZ German Research Center for Geosciences Potsdam Germany

4. Jet Propulsion Laboratory California Institute of Technology Pasadena California USA

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

6. Institute of Earth and Environmental Science University of Potsdam Potsdam‐Golm Germany

7. Institute of Tectonic Studies, Department of Geological Sciences University of Texas El Paso Texas USA

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

9. School of Earth Science and Engineering Sun Yat‐Sen University Guangzhou China

10. Department of Earth Science and Engineering Hebei University of Engineering Handan China

Funder

National Science Foundation

Jet Propulsion Laboratory

Deutscher Akademischer Austauschdienst

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/2017GL073627

Reference68 articles.

1. Relatively recent construction of the Tien Shan inferred from GPS measurements of present-day crustal deformation rates

2. Late Cenozoic reorganization of the Arabia-Eurasia collision and the comparison of short-term and long-term deformation rates

3. Inverse and forward numerical modeling of trishear fault-propagation folds

4. Along-strike growth of the Ostler fault, New Zealand: Consequences for drainage deflection above active thrusts

5. Overlapping Faults, Intrabasin Highs, and the Growth of Normal Faults

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