Temporally constant slip rate along the Ganzi fault, NW Xianshuihe fault system, eastern Tibet-Reference-Cited by-同舟云学术

Temporally constant slip rate along the Ganzi fault, NW Xianshuihe fault system, eastern Tibet

Published:2017-09-12 Issue:3-4 Volume:130 Page:396-410
ISSN:0016-7606
Container-title:GSA Bulletin
language:en
Short-container-title:

Author:

Chevalier Marie-Luce¹,Leloup Philippe Hervé²,Replumaz Anne³,Pan Jiawei¹,Métois Marianne²,Li Haibing¹

Affiliation:

1. Key Laboratory of Continental Dynamics, Institute of Geology, Chinese Academy of Geological Sciences, 26 Baiwanzhuang Road, Beijing 100037, People’s Republic of China

2. Laboratoire de Géologie de Lyon, CNRS UMR 5570, Université de Lyon 1, 69622 Villeurbanne, France

3. Institut des Sciences de la Terre (ISTerre), Université Grenoble Alpes, 38058 Grenoble, France

Publisher

Geological Society of America

Subject

Geology

Link

http://pubs.geoscienceworld.org/gsa/gsabulletin/article-pdf/130/3-4/396/4084255/396.pdf

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4. A complete and easily accessible means of calculating surface exposure ages or erosion rates from 10Be and 26Al measurements;Balco;Quaternary Geochronology,2008

5. Cosmogenic nuclide dating of earthquakes, faults, and toppled blocks;Benedetti;Elements,2014

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