• 责任者：Feng Qianwen (Institute of Geology ; Chinese Academy of Geological Sciences ; Beijing 10037 ; China) ; Li Jinyi
• 刊名：Xinjiang Geology
• 出版年：2012
• 卷期：30(2)
• 关键词：走滑断层 ; strike-slip faults ; 左旋断层 ; left-lateral faults ; 新疆 ; Xinjiang
• 页码：p.132-135
• 图表：1 illus., 10 refs.
• 分类号：0300
• issnNo：ISSN1000-8845
• isbnNo：CN65-1092/P

Xingdi fracture zone is a major fracture, and different understanding about the tectonic history of this fracture exists. Considering there is no measurement about the Xingdi fracture, this study interprets the satellite remote sensing images and determines the geometry characteristics of this fracture. By determining the cut and displaced boundaries of Devonian sedimentary rocks, Carboniferous granite and granodiorite, and dyke swarm emplaced in them, a measurement of 8.26~9.19 km can be convinced as the sinistral strike-slip displacement of the Xingdi fracture.