Banno S,Enami M,Hirajima T,Ishiwateri A,Wang Q C.2000.Decompression P-T path of coesite eclogite to granulite from Weihai,eastern China.Lithos,52:97～108.
[5]
Finch R J,Hanchar J M.2003.Structure and chemistry of zircon and zircon-group minerals.Reviews in Mineralogy and Geochemistry,53:1～25.
[6]
Gebauer D,Lappin M,Grunenfelder M,Wyttenbach A.1985.The age and origin of some Norwegian eclogites:a U-Pb zircon and REE study.Chemical Geology,52:227～247.
[7]
Hazen R M,Finger L W.1979.Crystal structure and compressibility of zircon at high pressure.American Mineralogist,64:196～201.
[8]
Hirajima T,Ishiwateri A,Cong B L,Zhang R Y,Banno S,Nozaka T.1990.Identification of coesite in Mengzhong eclogite from Donghai county,northeastern Jiangsu Province,China.Mineralogical Magazine,54:579～584.
[9]
Hoskin P W O,Schaltegger U.2003.The composition of zircon and igneous and metamorphic petrogenesis.Reviews in Mineralogy and Geochemistry,53:27～62.
[10]
King E M,Valley J W,Davis D W,et al.1998.Oxygen isotope ratios of Archean plutonic zircons from granite-greenstone belts of the Superior Province:Indicator of magmatic source.Precambrian Research,92:365～387.
[11]
Liu F L,Xu Z Q,Katayama I,et al.2001.Mineral inclusions in zircons of para-and orthogneiss from pre-pilot drillhole CCSD-PP1,Chinese Continental Scientific Drilling Project.Lithos,59:199～215.
[12]
Liu F L,Xu Z Q,Liou J G,et al.2004.SHRIMP U-Pb ages of ultrahigh-pressure and retrograde metamorphism of gneiss,southwestern Sulu terrane,eastern China.Journal of Metamorphic Geology,22:315～326.
[13]
Peucat J J,Videl P,Godard G Postaire B.1982.Precambrian U-Pb zircon ages in eclogites and garnet pyroxenites from South Brittany (France):an old oceanic crust in the West European Hercynian belt? Earth and Planetary Science Letters,60:70～78.
[14]
Rubatto D,Gebauer G,Compagnoni R.1999.Dating of eclogite-facies zircons:the age of Alpine metamorphism in the Sesia-Lanzo Zone (Western Alps).Earth and Planetary Science Letters,167:141～158.
[15]
Spear F S.1995.Metamorphic phase equilibria and pressure-temperature-time paths.Monograph Series.Mineralogical Society of America,Washington,DC,USA,1～799.
[16]
Wang R C,Wang S,Qiu J S,Ni P.2005.Rutile in the UHP eclogites from the CCSD main drill hole (Donghai,eastern China):Trace-element geochemistry and metallogenetic implications.Acta Petrologica Sinica,21(2):465～474 (in Chinese with English abstract).
[17]
Wang S,Wang R C,Qiu J S,Ni P,Yu J J.2006.Mineral inclusions in rutile of Sulu UHP eclogites from the main drill hole of CCSD,Donghai.Acta Petrologica et Mineralogica,25 (1):61～70 (in Chinese with English abstract).
[18]
Watson E B,Harrison T M.2005.Zircon thermometer reveals minimum melting conditions on earliest earth.Science,308:841～844.
[19]
Wu Y B,Zheng Y F,Gong B,Zhao Z F.2005.Zircon U-Pb ages and oxygen isotope compositions for granite at Xinkailing in the Beihuaiyang zone and their significance.Earth Science-Journal of China University of Geosciences,30:659～672 (in Chinese with English abstract).
[20]
Valley J W,Chiarenzeli J R,McLelland J M.1994.Oxygen isotope geochemistry of zircon.Earth and Planetary Science Letters,126:187～206.
[21]
Ye K,Yao Y,Katayama I,Cong B L,Wang Q C,Maruyama S.2000a.Large area extent of ultrahigh-pressure metamorphism in the Sulu ultrahigh-pressure terrane of East China:new implications from coesite and omphacite inclusions in zircon of granitic gneiss.Lithos,52:157～164.
[22]
Zhang R Y,Hirajima T,Banno S,Cong B L,Liou J G..1995.Petrology of ultrahigh-pressure rocks from the southern Sulu region,eastern China.Metamorphic Geology,13:659～675.
[23]
Zhang Z M,Xu Z Q,Liu F L,You Z D,Shen K,Yang J S,Li T F,Chen S Z.2004.Geochemistry of eclogites from the main hole (100～2050m) of the Chinese Continental Scientific Drilling Project.Acta Petrologica Sinica,20 (1):27～42 (in Chinese with English abstract).
[24]
Zhang Z M,Xiao Y L,Xu Z Q,Hoefs J,Liu F L,Liou J G,Simon K.2006.UHP metamorphic rocks from the Chinese continental scientific drilling project:I.Petrology and geochemistry of the main hole (0～2,050m).Contributions to Mineralogy and Petrology,DOI 10.1007/s 00410-006-0080-9.
[25]
Zheng Y F,Fu B,Li Y L,et al.1998.Oxygen and hydrogen isotope chemistry of ultra high pressure eclogites from the Dabie Mountains and the Sulu terrane.Earth and Planet Science Letters,155:113～129.
Enami M,Zhang Q,Yin Y.1993.High-pressure eclogites in northern Jiangsu-southern Shangdong province,eastern China.Journal of Metamorphic Geology,11:589～603.
[31]
Gebauer D A.1996.P-T-t path for an (ultra-?) high-pressure ultramafic-mafic rock-association and its felsic country-rocks based on SHRIMP-dating of magmatic and metamorphic zircon domains.Example:Alp Arami (Central Swiss Alps).In:Earth Processes Reading the Isotopic Code.Geophysical Mono-graph,95:307～329.
[32]
Hacker B R,Ratshbacher L,Webb L,Ireland T,Walker D,Dong S W.1998.U/Pb zircon ages constrain the architecture of the ultrahigh-pressure Qinling-Dabie orogen.Earth and Planetary Science Letters,161:215～230.
[33]
Heaman L M,Bowins R,Crocket J.1990.The chemical composition of igneous zircon suites:implications for geochemical tracer studies.Geochimica et Cosmochimica Acta,54:1597～1607.
[34]
Katayama I,Zayakhstan A A,Maruyama S.2000.Progressive P-T records from zircon in Kokchetav UHP-HP rocks,northern Kazakhstan.The Island Arc,9:417～427.
[35]
Liou J G,Zhang R Y.1998.Petrogenesis of ultrahigh-pressure garnet-bearing ultramafic body from Maowu,the Dabie Mountains,central China.The Island Arcs,7:33～96
[36]
Liou J G,Hacker B R,Zhang R Y.2000.Into the forbidden zone.Science,287:1215～1216.
[37]
Liu Y J.1984.Element Geochemistry.Beijing:Science Press,1～548 (in Chinese).
[38]
Okay A I,Xu S,Sengor A M C.1989.Coesite from the Dabie Mountains eclogite,central China.European Journal of Mineralogy,1:595～598.
[39]
Rubatto D,Gebauer D.2000.Use of cathodoluminescence for U-Pb zircon dating by IOM Microprobe:Some examples from the western Alps.Cathodoluminescence in Geoscience.Springer-Verlag Berlin Heidelberg,Germany,373～400.
[40]
Sawka W N.1988.REE and trace element variation in accessory minerals and hornblende from the strongly zoned McMurry Meadows Pluton,California.Trans Roy Soc Edinburgh:Earth Science,79:157～168.
[41]
Wang X,Griffin W L,et al.2002.Morphology and geochemistry of zircons from late Mesozoic igneous complexes in coastal SE China:implications for petrogenesis.Mineralogical Magazine,66:235～251.
[42]
Wang X,Griffin W L.2004.Unusual Hf contents in metamorphic zircon from coesite-bearing eclogites of the Dabie Mountains,east-central China:implications for the dating of ultrahigh-pressure metamorphism.Journal of Metamorphic Geology,22:629～637.
[43]
Watson E B,Cherniak D J,Hanchar J M,Harrison T M,Wark D A.1997.The incorporation of Pb into zircon.Chemical Geology,141:19～31.
[44]
Watson E B,Wark D A,Thomas J B.2006.Crystallization thermometers for zircon and rutile.Contributions to Mineralogy and Petrology,151:413～433.
[45]
Xu Z Q,Zhang Z M,Liu F L,Yang J S,Tang Z M,Chen S Z,Chai Y C,Li T F,Chen F Y.2004.The structure profile of 0～1200 m in the main borehole,Chinese Continental Scientific Drilling and its preliminary deformation analysis.Acta Petrologica Sinica,20(1):53～72 (in Chinese with English abstract).
[46]
Yang J J,Jhan B M.2000.Deep subduction of mantle-derived garnet peridotites from the Su-Lu UHP metamorphic terrane in China.Journal of Metamorphic Geology,18:167～180.
[47]
Ye K,Cong B L,Ye D N.2000b.The possible subduction of continental material to depths greater than 200 km.Nature,407:734～736.
[48]
Zack T,Moraes R,Kronz A.2004.Temperature dependence of Zr in rutile:empirical calibration of a rutile thermometer.Contributions to Mineralogy and Petrology,148:471～488.
[49]
Zhang R Y,Liou J G,Cong B L.1994.Petrogenesis of garnet-bearing ultramafic rocks and associated eclogites in the Su-Lu ultrahigh-pressure metamorphic terrane,China.Metamorphic Geology,18:149～166.
[50]
Zhang Z M,You Z D,Han Y J,Sang L K.1996.Petrology,metamorphic process and genesis of the Dabie-Sulu eclogite belt,Eastern-Central China.Acta Geology Sinica,9:134～156.
[51]
Zhang Z M,Xiao Y L,Sen K,Gao Y J.2005.Garnet growth compositional zonation and metamorphic P-T path of the ultrahigh-pressure eclogites from the Sulu orogenic belt,eastern Central China.Acta Petrologica Sinica,21:809～818 (in Chinese with English abstract).
[52]
Zheng Y F,Wu Y B,Chen F K,et al.2004.Zircon U-Pb and oxygen isotope evidence for a large-scale 18O depletion event in igneous rocks during the Neoproterozoic.Geochimica et Cosmochimica Acta,68:4159～4179.
