剪褶皱(Shear fold),或称滑褶皱(Slip fold),在国内外教科书及地质词典等文献中均有介绍。这个概念是Spitz于1911年引入的。W.carey于1962年用一组卡片模拟剪褶皱作用,该模式至今仍被广泛应用,如D.M.Ragan(1973)(图1)、B.E.Hobbs(1975)、武汉地院等四院校合编的构造地质学(1979)等等。许多研究者认为剪褶皱是,岩层沿着 Shear fold, also known as slip fold, is introduced in textbooks such as textbooks and geological dictionaries at home and abroad. This concept was introduced by Spitz in 1911. W.carey used a set of cards in 1962 to simulate the effect of clipping and folding, which is still widely used till now. Examples are DMRagan (1973) (Figure 1), BEHobbs (1975) and Wuhan Institute of Geography Structural Geology (1979) and many more. Many researchers believe that folds are the formation along the rock