Gibbs A D. Linked fault families in basins formation[J]. Journal of Structural Geology, 1990,12(5-6) :795-803.
[10]
Pohn H A. Lateral ramps in the folded Appalachians and in overthrust belts worldwide-a fundamental element of thrust-belt architecture[J]. U. S. Geological Survey Bulletin,2000,2163:1-63.
[11]
Boyer S E. Sendimentary basin taper as a factor controlling the geometry and advance of thrust belts [J]. American Journal of Science,1995, 295: 1220-1254.
[12]
Marshak S,Flottmann T. Structure and origin of the Fleurieu and Nackara Arcs in the Adelaide fold-thrust belt,South Australia:salient and recess development in the Delamerian Orogen [J]. Journal of Structural Geology,1996, 18(7): 891-908.
[13]
Platt J P,Behrmann J H,Cunningham P C, et al. Kinematics of the Alpine arc and the motion history of Adria[J]. Nature,1989,337: 158-161.
[14]
Sandiford M,Paul E,Flottmann T. Sedimentary thickness variation and deformation intensity during basin inversion in the Flinders Ranges,South Australia[J]. Journal of Structural Geology,1998, 20(12): 1721-1731.
[15]
Hindle D,Burkhard M. Strain, displacement and rotation associated with the formation of curvature in fold belts:the example of the Jura arc [J]. Journal of Structural Geology, 1999, 21:1089-1101.
[16]
Hindle D,Besson O,Burkhard M. A model of displacement and strain for arc-shaped mountain belts applied to the Jura arc [J].Journal of Structural Geology,2000, 22: 1285-1296.
