Barth A P, Wooden J L, Coleman D S. 2001. SHRIMP-RG U-Pb zircon geochronology of Mesoproterozoic metamorphism and plutonism in the southwesternmost United States. The Journal of Geology, 109: 319～327.
[14]
Chopin C, Sobolev N V. 1995. Principal meralogic indicators of UHP in crustal rocks. In: Colem R G, Wang X, eds. Ultrhigh-Pressure Metamorphism. Cambridge: Cambridge University Presses, 96～133.
[15]
Dobrzhinetskaya L F, Green Ⅱ H W, Mitchell T E, Dickerson R M.2001. Metamorphic diamonds: Mechanism of groth and inclusion of oxides. Geology, 29: 263～266.
[16]
Eide E A, McWilliams M O, Liou J G. 1994. 40Ar/39Ar geochronology and exhumation of high-pressure to ultrahigh-pressure metamorphic rocks in east-central China. Geology(Boulder), 22: 601～604.
[17]
Hu N, Yang J, Zhao D. 1996. Sm-Nd isochron age of eclogite from northern Qinling Mountains. Acta Mineralogica Sinica, 16 (4):349～352. (in Chinese with English abstract)
[18]
Hu N, Zhao D, Xu G, Wang T. 1994. Discovery of coesite-bearing eclogite in North Qinling and its significance. Chinese Science Bulletin, 39(21): 2013. (in Chinese)
[19]
Jian P, Liu D, Yang W, Williams I S. 2000, Petrological study of zircons and SHRIMP dating of the Caledonian Xiongdian eclogite,northwestern Dabie mountains. Acta Geologica Sinica, 74:259～264. (in Chinese with English abstract).
[20]
Kroner A, Zhang G W, Sun Y. 1993. Granulites in the Tongbai area,Qinling belt, China: geochemistry, petrology, single zircon geochronology and implications for the tectonic evolution of eastern Asia. Tectonics 12: 245～255.
[21]
Li S G, Hart S R, Zheng S G, Liu D L, Zhang G W, Guo A L.1989. Timing of collision between north and south China blocks The Sm-Nd isotopic age evidence. Science China, 32:1393 ～1400.
[22]
Li S, Xiao Y, Liu D, Chen Y, Ce N, Zhang Z, Sun S S, Cong B,Zhang R, Hart S R, Wang X. 1993. Collision of the North China and Yangtze blocks and formation of coesite bearing eclogites:Timing and processes. Chemical Geology, 109: 89～ 111.
[23]
Liu L, Wang Y, Sun Y, Xiao P, Chen D, Luo J, Che Z. 2001. The ultrahigh-pressure (＞3.5 GPa) magnesite-bearing garnet lherzolite in Altyn Tagh, northwestern China. Abstract of the UHPM Workshop 2001, at Waseda University, Fluid/Slab/mantle Interactions and Ultrahigh-P Minerals, 294～ 297.
[24]
Meng Q R. Zhang G W. 1999. Timing of collision of the North and South China blocks: Controversy and reconciliation. Geology,27: 123～126.
[25]
Nasdala L, Massonne H J. 2000. Microdiamonds from the Saxonian Erzgebirge, Germany: in situ micro-Raman characterization.Eur. J. Mineral, 12: 495～498.
[26]
Rozen O, Zorin Y, Zayachkovsky A. 1972. A find of the diamonds within eclogites of the Precambrian Kokchetav massif. Doklady Academi Nauk SSSR, 203: 674～676.
[27]
Song S, Yang J. 2001. Sanidine + quartz inclusions in Dulan eclogites: evidence for UHP metamorphism on the north margin of the Qaidam basin, NW China. Acta Geologica Sinica, 75:180～185 (in Chinese with English abstract)
[28]
van Roermund H L M, Drury M R, Barnhoom A, Ronde A. 2000.Super-silicic garnet microstruetures from an orogenic garnet peridot ite, evidence for an ultra-deep (＞6 GPa) origin. Journal of Metamorphic Geology, 18 : 135 ～ 148.
[29]
Xu S, Okay A L, Sengor A, Su W, Liu Y, Jiang L. 1992. Diamond from the Dabie Shan metamorphic rocks and its implication for tectonic setting. Science, 256: 80～82.
[30]
Xu Z Q, Yang J S, Zhang J X. 1999. Comparison of the tectonic units on both sides of the Altyn Tagh fault and the mechanism of lithospheric shearing. Acta Geologica Sinica, 73: 193～205. (in Chinese with English abstract)
[31]
Yang J S, Xu Z Q, Li H B, Wu C L, Cui J W, Zhang J X, Chen W 1998. Discovery of eclogite at northern margin of Qaidam Basin,NW China. Chinese Science Bulletin, 43: 755 ～ 1760.
[32]
Yang J S, Xu Z Q, Song SG, Zhang J X, Wu C L, Shi R D, Li H B,Brunel M. 2001a. Discovery of coesite in the North Qaidam Early Paleozoic ultrahigh pressure (UHP) metamorphic belt,NW China: C. R. Acad. Sci. Paris, Sciences de la Terre et des planets / Earth and Planetary Sciences, 333: 719～724.
[33]
Ye K, Cong B, Ye D. 2000. The possible subduction of continental material to depths greater than 200 km. Nature, 407:734～736.
[34]
Zhai X, Day H W, Hacker B R, You Z. 1998. Paleozoic metamorphism in the Qinling orogen. Tongbai Mountains, central China. Geology, 26: 371～374.
[35]
Zhang J X, YangJS, Xu Z Q, ZhangZN, Li H B, ChenW. 2000.U-Ph and Ar-Ar ages of eclogites from the northern margin of the Qaidam basin, northwestern China. Journal of the Geological Society of China (Taiwan), 43: 161～169.
[36]
Zhang J X, Zhang Z M, Xu Z Q, YangJ S, CuiJ W. 1999. The ages of U Pb and Sm-Nd for eclogite from the western segment of Altyn Tagh tectonic belt--the evidences for existence of Caledonian orogenic root. Chinese Science Bulletin, 44: 1109～1112. (in Chinese with English abstract)
[37]
Zhang Z. You Z. Han Y, Shang L. 1995. Petrology, metamorphism and genesis of the Dabie-Sulu eclogite belt. Acta Geologica Sini ca, 69: 306～324. (in Chinese with English abstract)
Ames L, Tilton G. R, Zhou G. 1993. Timing of collision of the SinoKorean and Yangtze crotons: U-Pb zircon dating of coesite-bearing eclogites. Geology,21: 339～342.
[49]
Ames L, Zhou G, Xiong B. 1996. Geochronology and geochemistry of ultrahigh-pressure metamorphism with implications for collision of the Sino-Korean and Yangtze cratons, Central China. Tectonics, 15: 422～489.
[50]
Chavagnac V, Jahn B M. 1996. Coesite-bearing eclogites from the Bixiling Complex, Dabie Mountains, China: Sm-Nd ages, geochemical chracteristics and tectonic implications. Chemical Geology, 133: 29～51.
[51]
Dobrzhinetskaya L F, Eide E, Korneliussen A, Larsen R, Millege J,Posukhova T, Smith D S, Sturt B, Taylor W R, Tronnes R.1995. Diamond in metamorphic rocks of the Western Gneiss region in Norway. Geology, 23: 597～600.
[52]
Hacker B R, Ratschbacher L, Webb L, Ireland T, Walker D, Dong S. 1998. U/Pb zircon ages constrain the architecture of the ulrahigh-pressure Qinling-Dabie Orogen, China. Earth and Planetary Science Letters, 161: 215～230.
[53]
Hu N, Zhao D, Xu Y, Wang T. 1995. Petrography and metamorphism study on high-ultrahigh pressure eclogite from Guanpo area, northern Qinling Mountains. Journal of Mineralogy and Petrology, 15(4): 1～9.
[54]
Jian P, Yang W, Li Z, Zhou H. 1997. Caledonian eclogite in Xiongdian, west Dabie: Evidence in isotopic chronology. Acta Geologica Sinica, 71(2): 133～141.
[55]
Katayama I, Maruyama S, Parkinson C T, Terada K, Sano Y. 2001.Ion micro-probe U-Pb zircon geochronology of peak and retro grade stages of ultrahigh-pressure metamorphic rocks from the Kokchetav massif, northern Kazakhstan. Earth and Planetary Science Letters, 188: 185～198.
[56]
Liu R. Fan Q, Li H. 1994, Zircon U Pb dating of the Bixiling eclogite in Dabie and its geological significance. In: Ouyang Z. (ed) New Progress of Mineralogy, Petrology and Geochemistry in China. Publishing House of Lanzhou University, Lanzhou.
[57]
Massonne H J. 1999. A new occurrence of microdiamonds in quart zofeldspathic rocks of the Saxonian Erzgebirge, Germany and their metamorphic evolution. In:Nixon P H, ed. Proceedings of VIIth International Kimberlite Conferrence, Cape Town, 1998:533～539.
[58]
Mattauer M. Matte Ph, Malavieille J, Tapponnier P, Maluski H, Xu Zhiqin, Lu Yilun, Tang Yaoqin. 1985. Tectonics of the Qinling belt: Build up and evolution of eastern Asia. Nature, 317:496～500.
[59]
Matte P. 1998. Continental subduction and exhumation of HP rocks in Paleozoic orogenic belts: Uralides and Variscides. GFF, 120:209～222.
[60]
Mposkos Evripidis D, Kostopoulos Dimistris K. 2001. Diamond, former coesite and spersilicic garnet in metasedimentary rocks from the Greek Phodope: a new ultrahigh-pressure metamorphic province established. Earth and Planetary Science Letters, 192:497～506.
[61]
Sobolev N, Shatsky V. 1990. Diamond inclusions in garnets from metamorphic rocks: A new environment of diamond formation.Nature, 343: 742～746.
[62]
Xu B, Grove M, Wang C Q, Zhang L F, Liu S W. 2000. 40Ar/39Ar thermochronology from the northwestern Dabie Shan: constraints on the evolution of Qinling-Dabie orogenic belt, eastcentral China. Tectonophysics, 322: 279～301.
[63]
Xue F, Lerch M F, Kroner A, Reischmann T. 1996. Tectonic evolu tion of the East Qinling mountains, China, in the Palaeozoic: a review and new tectonic model. Tectonophysics, 253:271～284.
[64]
Yang J S, Xu Z Q, Song S G, Wu C L, Shi R D, Zhang J X, Wan Y S, Li H B, Jin X C, Jalivet M. 2000. Discovery of eclogite in Dulan, Qinghai Province and its significance for the HP-UHP metamorphic belt along the central orogenic belt of China. Acta Geologica Sinica, 74: 156～168. (in Chinese with English abstract)
[65]
Yang J S, Xu Z Q, Zhang J X, Chu J Y, Zhang R Y, Liou J G.200lb. Tectonic significance of caledonian high-pressure rocks in the Qilian-Qaidam-Altun mountains, NW China. The Geologi cai Society of American, Memoir 194: 151 ～ 170.
[66]
Ye B, Jian P, Xu J. 1993. Sujiahe convergent belt in northern Tong bai-Dabie orogen and its constitution and evolution. Publishing House of China University of Geoscience in Wuhan.
[67]
You ZD, HanYJ, YangWR, ZhangZM, WeiBZ, LuiR. 1996.The high-pressure and ultrahigh pressure metamorphic belt in the east Qinling and Dabie Mountains, China. China University of Geosciences Press, Wuhan: 1 ～ 150.
Zhang J X, Yang J S, Xu Z Q, Meng F C, Song S G, Li H B, Shi R D. 2002. Evidence for the ultrahigh-pressure metamorphism in Altun eclogite. Chinese Science Bulletin, 47: 231 ～ 234. (in Chinese with English abstract)
[70]
Zhang Z Q, Liu D Y, Fu G. 1994. Isotopic geochronology of the Metamorphic Rocks in North Qinling. Beijing:Geological Publishing House. 75～ 105.
