清流南部地区的滑脱构造

Detachment Structure in the Southern Part of Qingliu County, Fujian Province

清流南部及邻区广泛存在的加里东、印支期滑脱构造应是该区造山作用的一个重要方面，它们的形成、发展与分隔闽西北、闽西南两大构造单元的南平－宁化北东东向构造－岩浆带密切相关。

This peper focuses on the discussion of the detachment structures in the southern part of Qingliu County, Western Fujian. The detachment structures, widespread exposeded in the southern port of Qingliu County and its neighbour area, belong to the Caledonian and Indosinian stages and are an important part of orogenesis. The formation and development of the dearchment structures have close relations with the Naping-Ninghua structural and magmatic belt (NEE trending), which separates the northwestern Fujian tectonic units from the Southwestern Fujian tectonic units.