摘要
///The Quaternary active features and combination relation of NW-striking fault zone in the downstream area of Jiulongjiang in Fujian province are researched. The results show that: 1) the Guokeng-Jiangdong fault(F1), Zhukeng fault(F3) and Jinfeng-Damaoshan fault(F7) actived in early Quaternary(Q1-2). Daishanyan-Hengkeng fault (F6) actived in Early Quaternary and Late Pleistocene on different segments. The Fuchuangshan-Kangshan fault (F4) and Jiulongjiang (west stream) fault (F5) actived in early Late Pleistocene. The Haicang-Qiangyu fault (F2) actived in Late Pleistocene; and 2) the Guokeng-Jiangdongqiao fault and the Jinfeng-Damaoshan fault divided the research area into 3 blocks and formed the Structural Assemblage of Xiaotiankeng horst, Zhangzhou graben and Guojianshan horst.