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Denudation pattern across the Longriba fault system and implications for the geomorphological evolution of the eastern Tibetan margin

  • Published:2015-10 Issue: Volume:246 Page:542-557
  • ISSN:0169-555X
  • Container-title:Geomorphology
  • language:en
  • Short-container-title:Geomorphology

Author:

Ansberque Claire,Godard Vincent,Bellier Olivier,De Sigoyer Julia,Liu-Zeng Jing,Xu Xiwei,Ren Zhikun,Li Yong,Team A.S.T.E.R.

Funder

French Ministry of Superior Education and Research

French National Research Agency

INSU-CNRS

Publisher

Elsevier BV

Subject

Earth-Surface Processes

Reference106 articles.

1. Grain size-dependent 10Be concentrations in alluvial stream sediment of the Huasco Valley, a semi-arid Andes region;Aguilar;Quat. Geochronol.,2014

2. Field study of a highly active fault zone: the Xianshuihe fault of southwestern China;Allen;Geol. Soc. Am. Bull.,1991

3. Seismic strain rates in the central and eastern United States;Anderson;Bull. Seismol. Soc. Am.,1986

4. Differential exhumation in response to episodic thrusting along the eastern margin of the Tibetan Plateau;Arne;Tectonophysics,1997

5. The French accelerator mass spectrometry facility ASTER: improved performance and developments;Arnold;Nucl. Instrum. Methods Phys. Res. Sect. B Beam Interact. Mater. Atoms,2010
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