Late Quaternary Slip-rates and Slip Partitioning on the Southeastern Xianshuihe Fault System, Eastern Tibetan Plateau-Reference-Cited by-同舟云学术

Late Quaternary Slip-rates and Slip Partitioning on the Southeastern Xianshuihe Fault System, Eastern Tibetan Plateau

Published:2016-04 Issue:2 Volume:90 Page:537-554
ISSN:1000-9515
Container-title:Acta Geologica Sinica - English Edition
language:en
Short-container-title:Acta Geologica Sinica - English Edition

Author:

Guihua CHEN¹,Xiwei XU¹,Xueze WEN²,Yue-Gau CHEN³

Affiliation:

1. Key Laboratory of Active Tectonics and Volcano; Institute of Geology, China Earthquake Administration; Beijing 100029 China

2. Earthquake Administration of Sichuan Province; Chengdu 610041 Sichuan China

3. Department of Geosciences; National Taiwan University; Taipei 10617 Taiwan China

Publisher

Wiley

Subject

Geology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1111/1755-6724.12689/fullpdf

Reference49 articles.

1. Field study of a highly active fault zone: the Xianshuihe fault of southwestern China;Allen;Geological Society of America Bulletin,1991

2. Slip partitioning by elastoplastic propagation of oblique slip at depth;Bowman;Science,2003

3. Application of digital acrophotogrammetry in active tectonics;Chen;Earth Science-Journal of China University of Geosciences,2006

4. Late quaternary climate and geomorphology on the northeastern margin of Sichuan-Yunnan block and their tectonomorphologic significance;Chen;Quaternary Sciences,2010

5. Late Cenozoic uplift of southeastern Tibet;Clark;Geology,2005

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