Davis D M, Engelder T. The role of salt in fold-and-thrust belts [J]. Tectonophysics, 1985, 119: 67-88.
[2]
Buxtorf A. Prognosen und befunde beim Hauesnsteinbasis und Grenchenberg -tunnel und die geologie des Juragebirges [J]. Verhandlungen der Naturforschenden GeseUchaft in Basel, 1916, 27: 184-205.
[3]
De Sitter L U. Structural Geology[M]. New York: McGraw-Hill, 1956.
[4]
Laubscher H P. Fold development in the Jura[J]. Tectonophysics, 1977, 37: 337-362.
[5]
Donatella M, Heroin A K, Massimiliano R B. Structural evolution of a fold and thrust belt generated by multiple decollements: analogue models and natural examples from the Northern Apezmines (Italy)[J]. Journal of Structural Geology, 2006, 28: 185-199.
[6]
Hemin A K, Bruno C Vendeville. The effect of decoUement dip on geometry and kinematics of model accretionary wedges[J]. Journal of Structural Geology, 2003, 25: 1445-1450.
[7]
朱志澄.中国南方侏罗山式褶皱及其形成机制[J].地球科学,1983,3:45-53.
[8]
Yan D P, Zhou M F, Song H L, et al. A Mesozoic, thin-skinned to thick-skinned, multi-layer over-thrust system within the Yangtze Block (South China)[J]. Tectonophysics, 2003, 361: 239- 254.
