1 Zheng Y F. Metamorphic chemical geodynamics in continental subduction zones. Chem Geol, 2012, 328: 5-48
[2]
2 Wu Y B, Zheng Y F, Tectonic evolution of a composite collision orogen: An overview on the Qinling-Tongbai-Hong'an-Dabie-Sulu orogenic belt in central China. Gondwana Res, 2013, 23: 1402-1428
[3]
3 Zheng Y F, Xiao W J, Zhao G C. Introduction to tectonics of China. Gondwana Res, 2013, 23: 1189-1206
[4]
4 Zhang G W, Yu Z P, Sun Y, et al. The major suture zone of the Qinling orogenic belt. J Southeast Asian Earth Sci, 1989, 3: 63-76
[5]
5 Ratschbacher L, Hacker B R, Calvert A, et al. Tectonics of the Qinling (Central China): Tectonostratigraphy, geochronology, and deformation history. Tectonophysics, 2003, 366: 1-53
[6]
6 Dong Y P, Zhang G W, Neubauer F, et al. Tectonic evolution of the Qinling orogen, China: Review and synthesis. J Asian Earth Sci, 2011, 41: 213-237
[7]
7 Diwu C R, Sun Y, Liu L A, et al. The disintegration of Kuanping Group in North Qinling orogenic belts and Neo-proterozoic N-MORB. Acta Petrol Sin, 2010, 26: 2025-2038
[8]
8 Yan Q R, Wang Z Q, Yan Z, et al. Timing of the transformation from seafloor spreading on the south margin of the North China Block to subduction within the North Qinling orogenic belt. Acta Geol Sin, 2009, 84: 1563-1583
[9]
9 Liu X C, Jahn B M, Hu J, et al. Metamorphic patterns and SHRIMP zircon ages of medium-to high-grade rocks from the Tongbai orogen, central China: Implications for multiple accretion/collision processes prior to terminal continental collision. J Metamorph Geol, 2011, 29: 979-1002
[10]
10 Liu X C, Jahn B M, Li S Z, et al. U-Pb zircon age and geochemical constraints on tectonic evolution of the Paleozoicaccretionary orogenic system in the Tongbai orogen, central China. Tectonophysics, 2013, 599: 67-88
[11]
11 Zheng Y F, Fu B, Gong B, et al. Stable isotope geochemistry of ultrahigh pressure metamorphic rocks from the Dabie-Sulu orogen in China: Implications for geodynamics and fluid regime. Earth Sci Rev, 2003, 62: 105-161
[12]
16 Zhang J X, Yu S Y, Meng F C, et al. Paired high-pressure granulite and eclogite in collision orogens and their geodynamic implications. Acta Petrol Sin, 2009, 25: 2050-2066
[13]
17 Cheng H, Zhang C, Vervoort J D, et al. Timing of eclogite facies metamorphism in the North Qinling by U-Pb and Lu-Hf geochronology. Lithos, 2012, 136-139: 46-59
24 Cheng H, King R L, Nakamura E, et al. Transitional time of oceanic to continental subduction in the Dabie orogen: Constraints from U-Pb, Lu-Hf, Sm-Nd and Ar-Ar multichronometric dating. Lithos, 2009, 110: 327-342
[16]
25 Liu X C, Wu Y B, Gao S, et al. Zircon U-Pb and Hf evidence for coupled subduction of oceanic and continental crust during the Carboniferous in the Huwan shear zone, western Dabie orogen, central China. J Metamorph Geol, 2011, 29: 233-249
[17]
27 Mattauer M, Matte P, Malavieille J, et al. Tectonics of the Qinling belt: Build-up and evolution of eastern Asia. Nature, 1985, 317: 496-500
[18]
29 Liu F L, Liou J G. Zircon as the best mineral for P-T-time history of UHP metamorphism: A review on mineral inclusions and U-Pb SHRIMP ages of zircons from the Dabie-Sulu UHP rocks. J Asian Earth Sci, 2011, 40: 1-39
[19]
30 Wu Y B, Gao S, Zhang H F, et al. Timing of UHP metamorphism in the Hong'an area, western Dabie Mountains, China: Evidence from zircon U-Pb age, trace element and Hf isotope composition. Contrib Mineral Petrol, 155: 123-133
[20]
31 Enkin R J, Courtillot V, Leloup P, et al. The paleomagnetic record of Uppermost Permian, Lower Triassic rocks from the South China Block. Geophys Res Lett, 1992, 19: 2147-2150
[21]
32 Zhao X X, Coe R S. Paleomagnetic constraints on the collision and rotation of north and south China. Nature, 1987, 327: 141－144
[22]
12 Xue F, Lerch M F, Kroner A, et al. Tectonic evolution of the east Qinling Mountains, China, in the Palaeozoic: A review and new tectonic model. Tectonophysics, 1996, 253: 271-284
[23]
13 Wang H, Wu Y B, Gao S, et al. Continental origin of eclogites in the North Qinling terrane and its tectonic implications. Precambrian Res, 2013, 230: 13-30
15 Yang J S, Xu Z Q, Dobrzhinetskaya L F, et al. Discovery of metamorphic diamonds in central China: An indication of a >4000-km-long zone of deep subduction resulting from multiple continental collisions. Terra Nova, 2003, 15: 370-379
[26]
18 Shi Y, Yu J H, Tectonic evolution of the Qinling orogenic belt, Central China: New evidence from geochemical, zircon U-Pb geochro-nology and Hf isotopes. Precambrian Res, 2013, 231: 19-60
[27]
19 Wang H, Wu Y B, Gao S, et al. Eclogite origin and timings in the North Qinling terrane, and their bearing on the amalgamation of the South and North China Blocks. J Metamorph Geol, 2011, 29: 1019-1031
[28]
20 Bader T, Ratschbacher L, Franz L, et al. The Heart of China revisited, I. Proterozoic tectonics of the Qin Mountains in the core of supercontinent Rodinia. Tectonics, 2013, doi: 10.1002/tect.20024
23 Wang H, Wu Y B, Gao S, et al. Silurian granulite-facies metamorphism, and coeval magmatism and crustal growth in the Tongbai orogen, central China. Lithos, 2011, 125: 249-271
[31]
26 Wu Y B, Hanchar J M, Gao S, et al. Age and nature of eclogites in the Huwan shear zone, and the multi-stage evolution of the Qinling-Dabie-Sulu orogen, central China. Earth Planet Sci Lett, 2009, 277: 345-354
[32]
28 Li S G, Xiao Y L, Liou D L, et al. Collision of the North China and Yangtze Blocks and formation of coesite-bearing eclogites: Timing and processes. Chem Geol, 1993, 109: 89-111
[33]
33 Li S Z, Kusky T M, Zhao G C, et al. Two stage Triassic exhumation of HP-UHP terranes in the western Dabie orogen of China: Constraints from structural geology. Tectonophysics, 2010, 490: 267-293
