[1]Mandl G. Mechanics of tectonic faulting[M]. Amsterdam: Elsivier,1988.154～155
[2]Louden K E. Paleomagnetism of DSDP sediments, phase shifting of magnetic anomalities and rotations of the West Philippine Basin[J].Journal of Geophysical Research, 1977,82:2 898～3 002
[3]Hustonm R B, Fuller M. Paleomagnetc datafrom the Philippine Sea plate and their tectonic significance[J]. Journal of Geophysical Research,1991,96:6 073～6 098
[4]Fuller M, Haston R, Lin J, et al. Tertiary paleomagnetism of regions around the South China Sea[J]. Joumal of Southeast Asia Earth Science, 1991,6:161～184
[5]Tsunakawa H. Neogene stress field of the Japanese arc and its relation to ineous activity[J]. Tectonophysics, 1986,124:1～22
[6]Jongsma D, Barber A J.东亚构造与资源研究[M].徐志成,沈政威,顾云芳,等译.北京:地质出版社,1985.22～72
[7]张文佑.中国及邻区海陆大地构造[M].北京:科学出版社,1986.408～412
[8]许浚远.欧亚板块东缘新生代盆地成因:右行剪切拉分作用[J].石油与天然气地质,1999,20(3):187～191
[9]赵重远,刘池洋.华北克拉通沉积盆地形成与演化及其油气赋存[M].西安:西北大学出版社,1990.75～84
[10]Dorsey R J. Collapse of the Luzon volcanic arc during onset of arccontinent eollision: evidence from a Miocene-Pliocene unconformity,East Taiwan[J].Tectonics, 1992,11 (2): 177～185
[11]Letouzey J, Kimura M. Okinawa Trough, genesis of back-arc basin developing along a continental margin[J]. Tectonophysies, 1986,125:209～230
[12]马杏垣.1:400万中国及邻近海域岩石圈动力学图说明书[M].北京:地质出版社,1986.64～69
[13]Nakata T,Otsuki K,Khan S H.Active faults,stress field,and lplate motion along the Indo-Eurasian plate boundary[J]. Tectonophysics, 1990,181:83～95
[14]杨森楠,杨巍然.中国区域大地构造学[M].北京:地质出版社,1985.195～202
[15]Nishimura S, Suparka S. Tectonics of east Indonesia[J]. Tectonophysics, 1990,181:257～266
[16]Northrup C J, Royden L H. Motion of the Pacific plate relative to Eurasia and its relation to Cenozoic extension along the eastm margin of Eurasia[J]. Geology, 1995,23(8):719～722
[17]Moores M E, Twiss J R. Tectonics[M]. New York: W H Freeman and company, 1995.155～195