| Abstract: | Lishui movement is one of the important movements in the late peried of Yanshanian move ment, which refers to the diastrophism reflected by the angular discordance between Tiantai group and Younkang group. To the south of Lishui city, a NNE basin, i. e. Wunongkou basin, composed of Yougkang group, was angular discordantly underlying Tiantai group at the southern slope of Nanmingshan mountaini to the east of Lishui city, Tiantai group was angular discordantly overlyin Moshishan group at shuidong. It is undoubted that Lishoui movement happened after Yougkang group, but before the accumulation of Tiantai group. |
