• 责任者：Liu Xingwang (Lanzhou Base of Institute of Earthquake Science ; China Earthquake Administration ; Lanzhou 730000 ; China) ; Yuan Daoyang
• 刊名：Chinese Journal of Geology
• 出版年：2012
• 卷期：47(1)
• 关键词：走滑断层 ; strike-slip faults ; 滑移速率 ; slip rates ; 祁连山 ; Qilian Mountains
• 页码：p.51-61
• 图表：7 illus., 18 refs.
• 分类号：0300
• issnNo：ISSN0563-5020
• isbnNo：CN11-1937/P

Fodongmiao-Hongyazi in an important margin fault which developed at the middle part of the northern Qinlian Mountain and the south of Hexi-corridor, the main trending is NWW with length 110 km. The fault is a fault is a left-lateral reverse strike-slip fault during the Holocene periods, it is also the seismogenic fault of Hongyabao M7 1/4 earthquake in 1609. The activity of the fault formed a series of geomorphology like fault scarp, terrace and gully left-lateral. In this study, based on the detail field work, we choose the typical geomorphology cell carried on large scale differential GPS measure.