摘要
浦市—辰溪浅层叠瓦状推覆构造位于雪峰山弧形构造带的北西侧，主要由浦市、水并湾、辰溪三条推覆构造带组成，推覆体地层时代为石炭纪、二叠纪、三叠纪及侏罗纪。推覆滑动面呈缓波状弯曲，总体倾向南东，倾角５～４０°不等，推覆滑动面呈叠瓦式排列。原地岩层在推覆构造作用下发生不同程度的褶皱。
Situated in the north-west side of Xuefengshan arc-structural belt,Pushi-Chenxi shallower imbricate nappe structure consists of three nappe strucure belts : Pushi belt,Shuijingwan belt and Chenxi belt.The strata of the nappes belong to Carboniferous,Permian,Trassic and Jurassic Periods. The gliding plane of the nappe is in gentle undulation,dipping generally south-east with angles 5～40°,All gliding planes arrange in imbrication. Rock layers in situ have been folded in different extent under the action of nappe structure.
出处
《湖南地质》
1995年第1期31-33,30,共4页
Hunan Geology
