Zhang Bingliang, Liang Xiaohua, Jiang Pu. 1996: MICROSTRUCTURAL STUDIES OF FAULT GOUGE FROM XIANGSHAN-TIANJINGSHAN FAULT ZONE AND THEIR ENGINEERING GEOLOGICAL SIGNIFICANCE. JOURNAL OF ENGINEERING GEOLOGY, 4(3): 47-52.
Citation:
Zhang Bingliang, Liang Xiaohua, Jiang Pu. 1996: MICROSTRUCTURAL STUDIES OF FAULT GOUGE FROM XIANGSHAN-TIANJINGSHAN FAULT ZONE AND THEIR ENGINEERING GEOLOGICAL SIGNIFICANCE. JOURNAL OF ENGINEERING GEOLOGY, 4(3): 47-52.
Zhang Bingliang, Liang Xiaohua, Jiang Pu. 1996: MICROSTRUCTURAL STUDIES OF FAULT GOUGE FROM XIANGSHAN-TIANJINGSHAN FAULT ZONE AND THEIR ENGINEERING GEOLOGICAL SIGNIFICANCE. JOURNAL OF ENGINEERING GEOLOGY, 4(3): 47-52.
Citation:
Zhang Bingliang, Liang Xiaohua, Jiang Pu. 1996: MICROSTRUCTURAL STUDIES OF FAULT GOUGE FROM XIANGSHAN-TIANJINGSHAN FAULT ZONE AND THEIR ENGINEERING GEOLOGICAL SIGNIFICANCE. JOURNAL OF ENGINEERING GEOLOGY, 4(3): 47-52.
Fault movement has a complex and variable pattern and one segment of a great faultzone is usually a unit of rupture. In order to meet the needs for major engineering projects and strong earthquake predication, It is necessary to lacate which segment of a fault zone is active. We propose in this paper that the movement of middle segment of Xiangshan-Tianjingshan fault zone is mainly stick-slip and both its eastern and western segments show mainly stable-slip. On the basis of microstructural characteristics of fault gouge and the segment geometry.
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