Amies L, Zhou G Z, Xiong B C. 1996. Geochronology and isotopiccharacter of ultrahigh-pressure metamorphism with implicationsfor collision of the Sino-Korean and Yangtze cratons, centralChina. Tectonics, 15(2): 472～489.
[6]
Chen Daogong, Etuenne Deloule, Xia Qunke, Chen Hao. 2000. Preliminary U-Pb ion probe age determination of zircon fromgneisses, Northern Dabie Terrain. Acta Petrol. Sin., 16(2):199～202(in Chinese with English abstract).
[7]
Composton W, Willims L S, Kirschvink J L. 1992. Zircon U-Pb agesfor the Early Cambrian time scale. J. Geol. Soc. London, 149:171～184.
[8]
Deng Jinfu, Dai Shengqian, Wu Zongxu, Zhao Hailing, Du jianguo,Luo Zhaohua. 2000. Petrological structure and thermal structure of the Dabie Orogenic Belt and its geological implications.Acta Geological Sinica, 74(3):279～285(in Chinese with English abstract).
[9]
Gebauer D, Schertl H P, Brix M. 1997. 35 Ma old ultrahigh-pressuremetamorphism and evidence for very rapid exhumition in DoraMaria Massif, Western Alps. Lithos., 41: 5～24.
[10]
Mclaren A C, Gerald J D, Williams. 1994. The microstructure of zircon and its influence on the age determination from Pb/U isotopic ratios measured by ion microprobe. Geochim. Cosmochim. Acta, 58(2) :993～1005.
[11]
Mezger K, Krogstad E J. 1997. Interpretation of discordant U-Pb zircon ages: An evaluation. J. metamorphic Geol., 15:127～140.
[12]
万天丰.2001.中朝与扬子板块的鉴别特征.地质论评,47(1):57～63.
[13]
王清晨,从柏林.1998.大别山超高压变质带的大地构造框架.岩石学报,14(4):481～492.
[14]
Hacker B R, Ratschbacher L, Webb L, Ireland T, Walker D, DongS. 1998. U/Pb zircon ages constrain the architecture of the ultrahigh-pressure Qinling-Dabie Orogen, China. Earth Planet.Sci. Letters, 161:215～230.
[15]
Hanchar J M, Miller C F. 1993. Zircon zonation patterns as revealedby cathodoluminescence and backscattered electron images: Implications for interpretation of complex crustal histories. Chemical geology, 110: 1～13.
[16]
Okay A. 1993. Petrology of a diamond and coesite-bearing metamorphic terrain: Dabie Shan, China. Eur. J. Mineral, 5: 659～ 675.
[17]
Rowley D B, Xue F, Tucker R D, Peng Z X, Baker J, Davis A.1997. Ages of ultra high pressure metamorphism and protolithorthgneisses from the eastern Dabie Shan: U/Pb zircongeochronology. Earth Planet Science Letters, 151:191～20.
[18]
Rubatto D, Gebauer D, Fanning M. 1998. Jurassic formation andEocene subductions for the geodynamic evolution of the Centraland Western Alps. Contrib. Mineral Petrol., 132:269～287.
[19]
Stacey J S, Kramers J D. 1975 Approximation of terrestrial lead isotopeevolution by a two-stage model. Earth and Planetary ScienceLetters, 26: 207～221.
[20]
Vavra G, Gebauer D, Schmid R. 1996. Multiple zircon growth and recrystallization during polyphase Late Carboniferous to Triassicmetamorphism in granulites of the Ivrea Zone (Southern Alps):an ion microprobe (SHRIMP) study. Contrib. MineralPetrol , 122: 337～358.
[21]
Vavra G, Schmid R, Gebauer D. 1999. Internal morphology, habitand U-Th-Pb microanalysis of amphibole to granulite facies zircon: geochronology of the Ivren Zone(Southern Alps). Contrib. Mineral Petrol. , 134:380～404.
[22]
Wan T F. 2001. Distinctive characteristics of Sino-Korean and YangtzPlates. Geological Review, 47(1):57～63 (in Chinese withEnglish abstract).
[23]
Wang Q C, Cong B L. 1998. Tectonic framework of the ultrahighpressure metamorphic zone from Dabie Mountains. Acta Petrol.Sin., 14(4):481～492(in Chinese with English abstract).
[24]
Williams I S, Claesson S, 1987. Isotopic evidence for the Precambrianprovenance and Caledonian metamorphism of high grade paragneisses from the Seve Nappes, Scandinavian Caledonides. Contrib. Mineral Petrol., 97: 205～217.
[25]
Xu Shutong, Jiang Laili, Liu Yican. 1992. Teconic regime and evolution of Dabie Mountain (the part of Anhui Provence). Acta Geological Sinica, 59 (4):279～285 (in Chinese with English abstract ).
[26]
Xu S, Okay A, Ji S, Senger A M C, Su W, Liu Y, Jiang L. 1992.Diamond from the Dabie Shan metamorphic rock and its implication for tectonic setting. Sciences, 256: 80～82.
[27]
Xue F, Rowley D B, Tucker R D, Peng Z X. 1997. U-Pb ages ofgranitoid rocks in the north Dabie complex, eastern Dabieshan,China. J. Geol., 105:744～753.
[28]
Zhai M, Cong B, Zhao Z, et al. 1995. Petrotectonic units in coesitebearing metamorphic terrain in the Dabie Mountains, centralChina and their geotectonic implications. Jour. Southeast AsianEarth Sci., 1:1～13.
[29]
Zheng Xiangshen, Jin Chengwei, Zhai Mingguo, Shi Yonghong.2000. Approach to the source of the gray gneisses in NortrhDabie Terrain: Sm-Nd isochron age and isotope composition.Acta Petrol. Sin., 16(2):194～198(in Chinese with Englishabstract).
