Allen M B, Macdonald D I M, Zhao X, Vincent S J and Brouetmenzies C. 1997. Early Cenozoic two-phase extension and late Cenozoic thermal subsidence and inversion of the Bohai Basin, northern China. Marine and Petroleum Geology, 14(7-8): 951?972.
[33]
Allen M B, Macdonald D I M, Zhao X, Vincent S J and Brouetmenzies C. 1998. Transtensional deformation in the evolution of the Bohai Basin, northern China // Holdsworth RE, Strachan R A and Dewey J E. Continental Transpressional and Transtensional Tectonics. Geological Society, London, Special Publications, 135: 215?229.
[34]
Engebretson D C, Cox A and Gordon R G. 1985. Relative motions between oceanic and continental plates in the Pacific Basin. Geological Society of America Special Paper, 206: 59.
[35]
Maruyama S, Isozaki Y, Kimura G and Terabayashi M. 1997. Paleogeographic maps of the Japanese Islands: Plate tectonic synthesis from 750 Ma to the present. Island Arc, 6: 121?142.
[36]
Mckenzie D. 1978. Some remarks on the development of sedimentary basin. Earth and Planetary Science Letters, 48(1): 25?32. doi: 10.1016/0012-821X(78)90071-7.
[37]
Menzies M A, Fan W M, Zhang M. 1993. Palaeozoic and Cenozoic lithoprobes and the loss of >120 km Archean lithosphere, Sino-Korean craton, China. Geological Society, London, Special Publication, 76: 71?81.
[38]
Qi J F and Yang Q. 2010. Cenozoic structural deformation and dynamic processes of the Bohai Bay basin province, China. Marine and Petroleum Geology, 27: 757?771.
[39]
Ren J Y, Tamaki K, Li S T and Zhang J X. 2002. Late Mesozoic and Cenozoic rifting and its Dynamic setting in Eastern China and adjacent areas. Tectonophysics, 344(3-4): 175?203.
[40]
Schellart W P and Lister G S. 2005. The role of the East Asian active margin in widespread extensional and strike-slip deformation in East Asia. Journal of the Geological Society, 162(6): 959?972. doi: 10.1144/0016- 764904-112.
[41]
Sengor A M C and Burke K. 1978. Relative timing of rifting and volcanism of Earth and its tectonic implications. Geophysical Research Letters, (5): 419?421.