Bhatia M R.1985. REE geochemistry of Australian Paleozoic graywackes and mudrocks: provenance and tectonic control. Sed. Geol. , 45: 97-113.
[17]
Chen T Y, Niu B G, Liu Z G, et al. 1991. Geochronology of Yanshanian magmatism and metamorphism in the hinterland of the Dabie mountains and their geologic significance. Acta Geologica Sinica, 65(4): 329-336 (in Chinese with English abstract).
[18]
Cong B L, Wang Q C. 1999. Recent development in study of Dabie-Sulu UHP rocks. Chinese Science Bulletin, 44:1127-1141 (in Chinese).
[19]
Dai S Q, Xu J C, Shi Q H, et al. 1992. New recognition of the Foziling Group in the eastern part of Northern Huaiyang. Regional Geology of China, (4): 369 -375 (in Chinese with English abstract).
[20]
Gao L D, Liu Z G. 1988. New discovery of microfossils from the Nanwan Formation of the Xinyang Group, Herren and its geological significance. Geological Review, 34 (5): 421 (in Chinese with English abstract).
[21]
Gao S, Zhang B R, Gu X M, et al. 1991. Silurian-Devonian coupling of the north China and Yangtze plates: evidence from the geochemistry of sedimentary rocks. Science in China (series B), 34:1372-1380.
[22]
Li S G, Liu D L, Chen Y Z, et al. 1994. Nd isotopic compositions of continental crust in the northern margin of Yangtze block and its tectonic implications. Geochimica, 23 (supp.): 10- 17 (in Chinese with English abstract).
[23]
Li S G, Han W L, Huang F, et al. 1998. Sm-Nd and Rb-Sr ages geochemistry of volcanics from the Dingyuan Formation in Dabie Mountains, central China: evidence to the Paleozoic magmatic arc. Scientia Geologica Sinica, 7: 461-470.
[24]
Ling W L, Gao S, Zhen H F, et al. 1998. An Sm-Nd isotopic dating study of the Archean Kongling complex in Huangling area of the Yangtze Craton. Chinese Science Bulletin, 43: 1187-1190.
[25]
Liu Z G, Niu B G, Ren J S. 1992. Disintegration of the Xinyang Group and its tectonic implication. Geological Review, 38 (4):293-301 (in Chinese with English abstract).
[26]
Mezger J E, Creaser R A. Erdmer P, et al. 2001. A Cretaceous back-arc basin in the coast belt of the northern Canadian Cordillera,evidence from geochemical and neodymium isotope characteristics of the Kluane metamorphic assemblage, southwest Yukon. Can. J. Earth Sci. , 38: 91-103.
[27]
Okay A I, Sengor A M C, Stair M. 1993. Tectonics of an ultrahigh-pressure metamorphic terrene: the Dabie Shan/Tongbai Shanorogen, China. Tectonics, 12:1320-1334.
[28]
Suo S T, Zhong Z Q, You Z D. 2000. Location of Triassic tectonic suture line between collided Sino-Korean and Yangtze cratons in Dabie--Sulu tectonic zone. Earth Sciences, 25: 111- 116 (in Chinese).
[29]
Wang R N, Wang D, Ouyang S. 1994. New knowledge of the Carboniferous systems in the northern slope of the Dabie Mountains. Journal of Stratigraphy, 18 (1): 17-23(in Chinese).
[30]
Wu W P, Xu S T, Jiang L L, et al. 2000. Deformation history of the UHPM complex in the Guazhen area, Tongcheng, eastern Dabie Mountains. Geology of Anhui, 10:199-204 (in Chinese).
[31]
Xu B, Wang C Q. 2000. Tectonic units in the western Dabie orogenic belts. Geological Journal of China Universities, 6:389-395 (in Chinese with English abstract).
[32]
Xu Q D, Ouyang J P, Zhang B R, et al. 2002. Tectonic affinity of Paleozoic stratigraphic slices along the northern margin in Dabie Orogen,central China: evidence from Pb isotope of rocks.Progress in Natural Science(English edition), 12: 438-444.
[33]
Xu S T, Jiang L L,Liu Y C,et al. 1992. Tectonic framework and -evolution of the Dabie Mountains in Anhui, Eastern China. Acta Geologica Sinica, 66(1):1 - 14 (in Chinese with English abstract).
[34]
Ye B D, Jian P, Xu J W, et al. 1993. The Sujiahe Terrene Collage Belt and Its Constitution and Evolution along the North Hillslope of the Tongbai-Dabie Orogenic Belt. Wuhan: Press of China University of Geoseienees, 5-54 (in Chinese).
[35]
Zhang G W, Meng Q R, Yu Z P, et al.1996. Orogenesis and dynamics of the Qinling Orogen. Science in China (Ser. D), 26 :193-200 (in Chinese).
[36]
Zhang Z Q, Liu D Y, Fu G M. 1994. Isotopic Dating of Metamorphic Stratigraphy in North Qinling Area. Beijing: Geological Publishing House, 1-119 (in Chinese).
[37]
Liu S F, Zhang G W, Cheng S Y, et al. 1999. Evolution of flexural basin and process of collision orogeny in east Qinling-Dabie Shan and its adjacent regions. Scientia Geologica Sinica, 34:336-346(in Chinese with English abstract).
Bhatia M R, Crook K A W. 1986. Trace element characteristics of greywackes and tectonic setting discrimination of sedimentary basins. Contrib. Mineral Petrol. , 92 : 181- 193.
[52]
Condie K C, Wilks M, Rosen D M, et al.1991. Geochmistry of metasediments from the Precambrian Hapschan Series, eastern Anabar Shield, Siberia. Precambrian Res., 50: 37-47.
[53]
Creaser R A, Erdmer P. 1997. Tectonic affinity of Nisutlin and Anvil assemblage strata from the Teslin tectonic zone, northern Canadian Cordillera: constraints from neodymium isotope and geochemical evidence. Tectonics, 16:107-121.
[54]
Farmer G L, Ball T T. 1997. Sources of Middle Proterozoic to Early Cambrian siliciclastic sedimentary rocks in the Great Basin: a Nd isotope study. GSA Bulletin, 109: 1193-1205.
[55]
Feng R, Kerrich R, Maas R. 1993. Geochemical,oxygen, and neodymium isotope compositions of metasediments from the Abitibi greenstone belt and Pontiac Subprovince, Canada: Evidence for ancient crust and Archean terrane juxtapodition. Geochim. Cosmochim. Acta, 57.-641-658.
[56]
Hao J, Liu X H. 1988. The large thrust-decollement structure and its evolution of Tongbai-Dabie collision type orogenic belt. Scientia Geologica Sinica, (1) : 1-10 (in Chinese with English abstract).
[57]
Hu S H, Chen A F, Lin S L, et al. 2000. ICP-MS analytical research into 40 trace and ultra-trace elements in geological samples. Earth Sciences, 25:186-190 (in Chinese with English abstract).
[58]
Ling W L, Gao S, Zhang B R, et al. 2000. The recognizing of ca. 1.95 Ga tectono-thermal event in Kongling nuelea and its significance for the evolution of Yangtze Block, south China. Chinese Science Bulletin, 46:26-329.
[59]
Liu W C, Wang G S. 1999. Mesozoic thrust and nappe tectonics in Northern Huaiyang region. Geosciences, 13: 143 - 149 (in Chinese).
[60]
Ma W P. 1991. The Carboniferous at the northern foot of the Dabie mountains and its tectonic implications. Acta Geologica Sinica, 65(1): 17-26 (in Chinese with English abstract).
[61]
McLennan S M, Taylor S R, McCulloch M T, et al. 1990. Geochemical and Nd-Sr isotopic composition of deep-sea turbidites:crustal evolution and plate tectonic associations. Geochim. Cosmochim. Acta, 54:2015-2050.
[62]
Niu B G, Fu Y L, Liu Z G. 1994. Main tectonothermal events and ^40Ar/^39Ar dating of the Tongbai-Dabie Mountains.Acta Geoscientia Sinica,68:20~34(in Chinese with English abstract).
[63]
Patchett P J, Roth M A, Canale B S, et al. 1999. Nd isotopes, geochemistry, and constraints on sources of sediments in the Franklinian mobile belt, Arctic Canada. GSA Bulletin, 111:578-589.
[64]
Roser B P, Korseh R J. 1986. Determination of tectonic setting of sandstone-mudstone suites using SiO2 content and K2O/Na2O ratio. J. Geol. , 94- 635-650.
[65]
Taylor S R, McLennan S M. 1985. The continental crust:Its composition and evolution. Cambridge: Blackwell.
[66]
Wimmenauer W. 1984. Das pravariskisehe Kristallin im Schwarzwald.Fortsehr. Miner. , 62: 69-86.
[67]
Xu S T, Liu Y S, Wu W P, et al. 2001. The major advance and problem of research in the Dabie orogenic belts. Progress in Natural Sciences, 11:796-803 (in Chinese).
[68]
Yang K G, Ma C Q, Yang W R. 1998. Significance of study of Mafan Caledonian intrusion in Beihuaiyang depression.Earth Sciences, 23:236-241 (in Chinese).
[69]
Zhang B R, Zhang H F, Zhao Z D, et al. 1996. Geochemical subdivision and evolution of the lithosphere in East Qinling and adjacent regions: Implications for tectonics. Science in China (Ser. D), 26:201-208 (in Chinese).