Characteristics of the Fault-Related Rocks, Fault Zones and the Principal Slip Zone in the Wenchuan Earthquake Fault Scientific Drilling Project Hole-1 (WFSD-1)
Tectonophysics 584 (2013) 23–42 Contents lists available at SciVerse ScienceDirect Tectonophysics journal homepage: www.elsevier.com/locate/tecto Characteristics of the fault-related rocks, fault zones and the principal slip zone in the Wenchuan Earthquake Fault Scientific Drilling Project Hole-1 (WFSD-1) Haibing Li a,b,⁎, Huan Wang a,b, Zhiqin Xu a,b, Jialiang Si a,b, Junling Pei a,c, Tianfu Li a,b, Yao Huang d, Sheng-Rong Song e, Li-Wei Kuo e, Zhiming Sun a,c, Marie-Luce Chevalier a,b, Dongliang Liu a,b a State Key Laboratory of Continental Tectonic and Dynamics, Beijing 100037, China b Institute of Geology, Chinese Academy of Geological Sciences, No.26, Baiwanzhuang Road, Beijing 100037, China c Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China d No.6 brigade of Jiangsu Geology & Mineral Resources Bureau, Lianyungang, Jiangsu, 222300, China e Department of Geosciences, National Taiwan University, Taipei, China article info abstract Article history: Scientific drilling in active faults after a large earthquake is ideal to study earthquake mechanisms. The Received 2 September 2011 Wenchuan earthquake Fault Scientific Drilling project (WFSD) is an extremely rapid response to the 2008 Received in revised form 12 August 2012 Ms 8.0 Wenchuan earthquake, which happened along the Longmenshan fault, eastern margin of the Tibetan Accepted 14 August 2012 Plateau. In order to better understand the fault mechanism and the physical and chemical characteristics of Available online 24 August 2012 the rocks, the WFSD project will eventually drill 5 boreholes along the two main faults. This paper focuses on the first hole (WFSD-1), which started just 178 days after the earthquake, down to a final depth of Keywords: fi Wenchuan earthquake fault scientific drilling 1201.15 m.
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