Variations of Lateral Bedrock Erosion Rates Control Planation of Uplifting Folds in the Foreland of the Tian Shan, NW China-Reference-Cited by-同舟云学术

Variations of Lateral Bedrock Erosion Rates Control Planation of Uplifting Folds in the Foreland of the Tian Shan, NW China

Published:2017-12 Issue:12 Volume:122 Page:2431-2467
ISSN:2169-9003
Container-title:Journal of Geophysical Research: Earth Surface
language:en
Short-container-title:J. Geophys. Res. Earth Surf.

Author:

Bufe Aaron¹²³^ORCID,Burbank Douglas W.¹²^ORCID,Liu Langtao⁴⁵^ORCID,Bookhagen Bodo²⁶^ORCID,Qin Jintang⁴,Chen Jie⁴^ORCID,Li Tao⁴⁷^ORCID,Thompson Jobe Jessica A.⁸^ORCID,Yang Huili⁴

Affiliation:

1. Department of Earth SciencesUniversity of California Santa Barbara CA USA

2. Earth Research InstituteUniversity of California Santa Barbara CA USA

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

4. State Key Laboratory of Earthquake Dynamics, Institute of GeologyChina Earthquake Administration Beijing China

5. Department of Earth Science and EngineeringHebei University of Engineering Handan China

6. Institute of Earth and Environmental ScienceUniversity of Potsdam Potsdam Germany

7. Department of Earth SciencesSun Yat‐Sen University Guangzhou China

8. Institute of Tectonic Studies, Department of Geological SciencesUniversity of Texas at El Paso El Paso TX USA

Funder

National Natural Science Foundation of China

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Earth-Surface Processes,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/2016JF004099

Reference168 articles.

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

2. Lithologic and tectonic controls on bedrock channel form at the northwest Himalayan front

3. Geomorphic constraints on listric thrust faulting: Implications for active deformation in the Mackenzie Basin, South Island, New Zealand

4. Explicit treatment of inheritance in dating depositional surfaces using in situ 10Be and 26Al

5. Exceptional river gorge formation from unexceptional floods

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