Tectonic evolution of the Tancheng-Lujiang(Tan-Lu) fault via middle Triassic to Early Cenozoic paleomagnetic data. Journal of Geophysical Research, 104(B7): 15365-15390.
[13]
Hacker B R, Ratschbacher L, Webb L, Ireland T, Walker D and Dong S W. 1998. U/Pb zircon ages constrain the architecture of the ultrahigh-pressure Qinling-Dabie orogen, China. Earth and Planetary Science Letters, 161(1-4): 215-230.
[14]
Hacker B R, Ratschbacher L, Webb L, Mcwilliams M O, Calvert A, Dong S, Wenk H R and Chateigner D. 2000. Exhumation of ultrahigh-pressure continental crust in east central China: Late Triassic-Early Jurassic tectonic unroofing. Journal of Geophysical Research, 105(B6): 13339-13364.
[15]
Hacker B R, Wallis S R, Ratschbacher L, Grove M and Gehrels G. 2006. High-temperature geochronology constraints on the tectonic history and architecture of the ultrahigh-pressure Dabie-Sulu Orogen. Tectonics, 25(5): 1-17.
[16]
Hsu K J, Wang Q C, Li J L, Zhou D and Sun S. 1987. Tectonic evolution of Qinling Mountains, China. Eclogae Geologicae Helvetiae, 80(3): 735-752.
[17]
Li S, Jagoutz E, Chen Y Z and Li Q L. 2000. Sm-Nd and Rb-Sr isotopic chronology and cooling history of ultrahigh pressure metamorphic rocks and their country rocks at Shuanghe in the Dabie Mountains, Central China. Geochimica et Cosmochimica Acta, 64(6): 1077-1093.
[18]
Li S, Xiao Y, Liu D, Chen Y, Ge Y, Zhang Z, Sun S S, Cong B, Zhang R, Hart S R and Wang S. 1993. Collision of the North China and Yangtze Blocks and formation of coesitebearing eclogites: Timing and processes. Chemical Geology, 109(1/4): 89-111.
[19]
Li Z X. 1994. Collision between the north and south blocks: A crust-detachment model for suturing in the region east of the Tan-Lu fault. Geology, 22: 739-742.
[20]
Watson M P, Hayward A B, Parkinson D N and Zhang Zh M. 1987. Plate tectonics history, basin development and petroleum source rock deposition onshore China. Marine and Petroleum Geology, 4(3): 205-225.
Chang E Z. 1996. Collision orogen between north and south China and its eastern extension in the Korean Peninsula. Journal of Southeast Asian Earth Sciences, 13(3): 267-277.
[30]
Chung S L. 1999. Trace element and isotope characteristics of Cenozoic basalts around the Tanlu fault with implications for the eastern plate boundary between north and south China. The Journal of Geology, 107(3): 301-312.
[31]
Gilder S A, Leloup P H, Courtillot V, Chen Y, Coe R S, Zhao X X, Xiao W J, Halim N, Cogne J P and Zhu R X. 1999.
[32]
Lin J L and Fuller M. 1990. Paleomagnetism, North and South China collision, and the Tan-Lu fault. Phil Trans Roy Soc Lond, A331: 589-598.
[33]
Okay A I and Sengor A M C. 1992. Evidence for intracontinental thrust related exhumation of the ultra-high-pressure rocks in China. Geology, 20(5): 411-414
[34]
Xu J W, Zhu G, Tong W X, Cui K R and Lin Q. 1987. Formation and evolution of the Tancheng-Lujiang wrench fault system: A major shear system to the northwest of the Pacific Ocean. Tectonophysics, 134: 273-310.
[35]
Yin A and Nie S Y. 1993. An indendation model for the North and South China collision and the development of the Tan-Lu and Honam fault system, eastern Asia. Tectonics, 12(4): 801-813.
[36]
Zhang K J. 1997. North and South China collision along the eastern and southern North China margins. Tectonophysics, 170(1): 145-156.
[37]
Zhang Q, Teyssier C, Dunlap J and Zhu G. 2007. Oblique collision between North and South China recorded in Zhangbaling and Fucha Shan (Dabie-Sulu transfer zone) // Till A B, Boeske S M, Sample J C and Foster D A. Exhumation Associated with Continental Strike-Slip Fault System. The Geological Society of America Special Paper, 434(9): 167-206
[38]
Zhang Z M, Liou J G and Coleman R G. 1984. An outline of the plate tectonics of China. Geological Society of America Bulletin, 95(3): 295-312.
[39]
Zhu G, Jiang D Z, Zhang B L and Chen Y. 2012. Destruction of the eastern North China Craton in a backarc setting: Evidence from crustal deformation kinematics. Gondwana Research, 22(1): 86-103.
[40]
Zhu G, Liu G S, Niu M L, Xie C L, Wang Y S and Xiang B W. 2009. Syn-collisional transform faulting of the Tan-Lu fault zone, East China. International Journal of Earth Sciences, 98(1): 135-155.
[41]
Zhu G, Niu M L, Xie C L and Wang Y S. 2010a. Sinistral to normal faulting along the Tan-Lu Fault Zone: Evidence for geodynamic switching of the East China continental margin. Journal of Geology, 118(3): 277-293.
[42]
Zhu G, Xie C L, Chen W, Xiang B W and Hu Z Q. 2010b. Evolution of the Hongzhen metamorphic core complex: Evidence for Early Cretaceous extension in the eastern Yangtze craton, eastern China. Geological Society of America Bulletin, 122: 506-516.
