Evolution of the in situ rock strain observed at Shandan monitoring station during the M8.0 earthquake in Wenchuan, China

Author:

Cai Meifeng,Peng Hua,Ma Xiumin,Jiang Jingjie

Publisher

Elsevier BV

Subject

Geotechnical Engineering and Engineering Geology

Reference8 articles.

1. Current tectonic activities in the intersection area of the Xianshuihe fault and Longmenshan fault in the eastern margin of the Qinghai-Tibet plateau;Tang;Geol Bull China,2005

2. Geomorphic evidence for the late Cenozoic strike-slipping and thrusting in Longmen mountain at the eastern margin of the Tibetan plateau;Li;Quat Sci,2006

3. Monitoring of active faults based on GPS with the Xianshuihe fault and Longmenshan fault as objective;Tang;J Mount Sci,2007

4. The intensity and epicenter of the M5.6 earthquake occurred in 2004 in Dong lake region of Tibet, China;Wu;Seismol Geol,2007

5. Comprehensive interpretation of seismic and geological data in the north section of Longmen mountain structural belts;Xiao;Nat Gas Ind,2005

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