Abstract
The Tongbai orogenic belt (TOB) is composed of six tectonic units. From south to north these units are: Tongbai gneiss rise (TGR); Hongyihe-Luozhuang eclogite belt (HLE); Maopo-Hujiazhai igneous rock belt (MHI); Zhoujiawan flysch belt (ZFB); Yangzhuang greenschist belt (YGB); and Dongjiazhuang marble belt (DMB). The geometry and kinematic images of the TOB include: the antiformal structures caused by a later uplift process, the top-to-north ductile shear structure that related to a process that the ultrahigh pressure rocks are brought to surface, the top-to-south ductile shear thrust and the sinistrial shear structures related to a south-north direction compression, and the east-west direction fold structures in the upper crust. In the view of the multistage subduction-collision orogenic belt, according to the characters of petrology and its distribution, geometry, kinematics and structural chronology in these tectonic units, tectonic evolution of the TOB can be divided into four stages: oceanic crust subduction during 400–300 Ma, continental collision during 270–250 Ma, continental deep subduction and uplift during 250–205 Ma and doming deformation during 200–185 Ma.
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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
Zhang G W, Meng Q R, Yu Z P, et al. The geodynamics and evolution of Qinling orogen. Sci China Ser D-Earth Sci (in Chinese), 1996, 3: 193–200
Zhang G W, Zhang B R, Yuan X C, et al. Qinling Orogen Belt and Continent Dynamics. Beijing (in Chinese): Science Press, 2001. 421–722.
Wang Q C, Cong B L. Tectonics of Dabie UHP metamorphose belt. Acta Petrol Sin (in Chinese), 1998, 14(4):481–492.
Xu B, Wang C Q. Tectonic units of Western Dabie orogen. Geol J Chin Univ (in Chinese with English abstract), 2000, 3: 389–395
Huang S Y, Wang Z M, Xu B. Basical Geometric and Kinematic analysis of Southwestern Dabie orgen. Geotectonic and Metallogenia (in Chinese with English abstract), 2002, 26(3): 240–246
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.
Kröner A, Zhang G W, Sun Y. Granulites in the Tongbai area, Qinling belt, China: geochemistry, petrology, single zircon geochronology, and implications for the tectonic evolution of eastern Asia. Tectonics, 1993, 12: 245–255
Li SG, Huang F, Nie Y H, et al. Geochemical and geochronological constraints on the suture location between the north and south China blocks in the Dabie orogen, central China. Phys Chem Earth (A), 2001, 26: 655–672
Hacker B R, Ratschbacher L, Webb L, et al. Exhumation of the ultrahigh-pressure continental crust in east-central China: Late Triassic-Early Jurassic extension. JGR, 2000, 105: 13339–13364
Webb L E, Hacker B R, Ratschbacher L, et al. Thermochronologic constraints on deformation and cooling history of high-and ultra-high-pressure rocks in the Qinling-Dabie orogen, eastern China. Tectonics, 1999, 18(4): 621–638
Suo S T, Zhong Z Q, Zhang H F, et al. High pressure metamorphic belt and its tectonic pattern in Tongbai Mountain, Central China. J Chin Univ Geosci (in Chinese with English abstract), 2001, 26(6): 551–559
Zhong Z Q, Suo S T, Zhang H F, et al. Major constituents and texture of the Tongbai-Dabie collisional orogenic belt. J Chin Univ Geosci (in Chinese with English abstract), 2001, 26(6):560–567
Li S G, Han W, Huang F. Sm-Nd and Rb-Sr ages and geochemistry of volcanics from the Dingyuan Formation in Dabie Mountains, central China: evidence to the Paleozoic magmatic arc. Sci Geol Sin, 1998, 7(4): 461–470
Liu Z G, Fu Y L, Niu B G, et al. Ar/Ar age of Sujiahe group and Guishan formation basicty complex and its geological implications, Northern Dabie. Chin Sci Bull (in Chinese), 1993, 38(13): 1214–1218
Zhang R J, Shu D G, Jiang Z W, et al. Cambrian Bradoriids from Caijia’ao marble body, Tongbai, Henan and their Geological significance. Geol Rev (in Chinese with English abstract), 2000, 46(3): 225–231
Feng Q L, Du Y S, Zhang Z H, et al. Early Triassic Radiolatian Fauna of Tongbai region in Henan and its geological significance. J Chin Univ Geosci (in Chinese with English abstract), 1994, 19(6): 787–794
Zhai X, Day H W, Hacher B R, et al. Paleozoic metamorphism in the Qinling orogen, Tongbai Mountains, Central China. Geology, 1998, 26: 371–374
Faure M, Lin W, Schärer U, et al. Continental subduction and exhumation of UHP rocks, Structural and geochronological insights from the Dabieshan (East China). Lithos, 2003, 70: 213–241
Xu B, Marty G, Wang C Q, et al. 40Ar/39Ar thermochronology from the northwestern Dabie Shan: constraints on the evolution of Qinling-Dabie orogenic belt, east-central China. Tectonophysics, 2000, 322: 279–301
Li S G, Hart S R, Zheng G, et al. Timing of collision between the north and south China blocks: the Sm-Nd isotopic age evidence. Sci China Ser B-Chem, 1989, 32: 1391–1400
Ye K, Cong B L, Ye D N, The possible subduction of continental material to depths greater than 200 km. Nature, 2000, 407(12): 734–736
Eide E A, McWilliams M O, Liou J G. 40Ar/39Ar method geochronology and exhumation of high-pressure to ultrahigh-pressure metamorphic rocks in east-central China. Geology, 1994, 22: 601–604
Lerch M F, Xue F, Kröner A, et al. A middle Silurian-early Devonian magmatic arc in the Qinling Mountains of central China. J Geol, 1995, 103: 437–449
Shi Q Z, Mou Y J, Zhang E H, et al. Decrease complex of Xinyang, Henan. Seism Geol (in Chinese), 1982, 4(1): 11–21
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Huang, S., Xu, B., Wang, C. et al. Geometry, kinematics and evolution of the Tongbai orogenic belt. SCI CHINA SER D 49, 828–838 (2006). https://doi.org/10.1007/s11430-006-0828-0
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DOI: https://doi.org/10.1007/s11430-006-0828-0