ZHOU M F;ROBINSON P T;MALPAS J;LI Z,Podiform chromitites in the Luohusa Ophiolite (southern Tibet):implications for melt-reck interaction and chromite segregation in the upper mantle,Journal of Petrology,1996(01).
[3]
ZHONG Lifeng;XIA Bin;ZHANG Yuquan;WANG Ran WEI Dongliang YANG Zhiqing,SHRIMP Age Determination of the Diabase in Luubusa Ophiolite,Southern Xizang (Tibet),Geological Review,2005.
[4]
鲍佩声;肖序常;王军,西藏中北部双湖地区蓝片岩带及其构造涵义,地质学报,1999(04).
[5]
LIU L G,Silicate perovskite from phase transformation of pyopegarnet at high pressure and temperature,Geophysical Research Letters,1974.
白文吉;Paul T Robinson;方青松;杨经绥 颜秉刚 张仲明 胡旭峰 周美夫.西藏罗布莎豆荚状铬铁矿中的合金成分[J].地质学报,2003(05)
[8]
王希斌;鲍佩声;邓万明,西藏蛇绿岩,北京:地质出版社,1987.
[9]
BAI Wenji;YANG Jingsui;FANG Qingsong;YAN Binggang ZHANG Zhangming REN Yufeng SHI Nicheng MA Zbesbeng DAI Mingquan,Some native metals from ophiolitic chromitites in Tibet,Earth Sciences Frontiers,2007(01).
[10]
BAI wenji;YANG jingsui;FANG qingsang;YAN binggang,ZHANG Zhongming,REN Yufeng,SHI Nicheng,MA Zbesheng,DAI Mingquan,Study on a storehouse of ultra pressure mantle minerals-Podiform chromite deposits,Earth Science-journal of China University of Geosciences,2001(03).
[11]
XU S;OKAY A L;SENGOR A;SU W LIU Y JIANG L,Diamond from the Dabie Sben metamorphic rocks and its implication for tectonic setting,Science,1992.
[12]
XIAO Xuchang;WANG Fangguo,An introduction to the ophiolite of China,Bulletin of the Chinese Academy of Geological Sciences,1984(09).
[13]
WILDING M C;HARTE B;HARRIS J W,Evidence for a deep origin for Sao Luiz diamonds,Araxa,Brazil,1991.
[14]
WANG Hengsheng;BAI Wenji;WANG Xibin,Chromite Deposits and Their Genesis in China,北京:科学出版社,1983.
[15]
TAYLOR W R;MILLEDGE H J;GRIFFIN B J;NIXON P H,KAMPERMAN M,MATTEY D P,Characteristics of microdiamonds from ultramafic massifs in Tibet:authentic ophiolitic diamonds or contamination,1995.
STISSHOV S M;POPOVA S V,A new dense modification of silicas,Geokhimiya,1961.
[18]
SCOTTSMITH B H;DANCHIN J W;HARRIS J W;STRCCHE K J,Kimberlites near Orrorrce,South Australia,Amsterdam:Elsevier,1984.
[19]
MOORE R O;GURNEY J J,Pyroxene solid solution in garnets included in diamond,Nature,1985.
[20]
MC-CAMMONA C A;STACHELB T;HARRISC J W,Iron oxidation state in lower mantle mineral assemblages Ⅱ.Inclusions in diamonds from Kankan,Guinea,Earth and Planetary Science Letters,2004.
[21]
MALPAS J;ZHOU M F;ROBINSON P T;REYNOLDS P,Geochemical and geochronological constraints on the origin and emplacement of the Yarlung-Zangho ophiolites,Southern Tibet.In Ophiolites in Geological History,Geological Society of London Special Publication,2003.
[22]
LIU L G,Post-oxide phases of olivine and pyroxenc and mineralogy of the re,retie,Nature,1975.
[23]
Werner Joswig ;Thomas Stachel ;Jeff W. Harris ;Werner H. Baur ;Gerhard P. Brey,New Ca-silicate inclusions in diamonds—tracers from the lower mantle,Earth and Planetary Science Letters?,1999, 173(1-2).
[24]
HELMBERGER D;LAY T;NI S;GURNIS M,Deep mantle structure and the postperovskite phase transition,Proceedings of the National Academy of Sciences(USA),2005.
[25]
HAGGERTY S E,Superkimberlitos:a geodynamic diamond window to the Earth\'s core,Earth and Planetary Science Letters,1994(1-2).
[26]
GOARANT F;GUYOT F;PEYRONNEAU J;POIRIER J P,High-pressure and high-temperature reactions between silicates and liquid iron alloys,in the diamond anvil cell,studied by analytical electron microscopy,Journal of Geophysical Research-B:Solid Earth and Planets,1992(04).
[27]
Tibor Gasparik ;Mark T. Hutchison,Experimental evidence for the origin of two kinds of inclusions in diamonds from the deep mantle,Earth and Planetary Science Letters?,2000, 181(1-2).
[28]
Diamond Research Group of Institute of Geology;Chinese Academy of Geological Sciences,Discovery of diamond in Alpine ultramaric rocks of Tibet,Geological Review,1981.
[29]
CRAWFORD A J;FALLOON T J;GREEN D H,Clarification,petrogenesis and tectonic setting of Boninites,London:Unwin and Hyman,1989.
[30]
CONDIE Kent C,Mantle Plumes and Their Record in Earth History,Cambridge:Cambridge University Press,2001.
[31]
CHEN M;Goresy A;GILLET P,Ringweodite lamellae in olivine:Clues to olivine-ringwcodite phase transitian mechanisms in shocked meteorites and subducting slabs,Proceedings of the National Academy of Sciences(USA),2004.
CHEN M;SHARP T G;GORESY A E;WOPENKA B XIE X,The majorite-pyrope+magnesiowustite assemblage:constraints on the history of shock verins in Chandrite,Science,1996.
[34]
BAO Peisbeng;XIAO Xnehang;WANG Jun,The blueschist belt in the Shuanghu region,Central-nortbern Tibet and its tectonic implications,Acta Geologica Sinica,1999(04).
[35]
BAI Wenji;SHI Nieheng;YANG Jingsui;FANG Qingsong REN Yufeng RONG He LI Guowu MA Zhesbeng.An assemblage of simple oxide minerals from ophiolitic pediform chromitites in Tibet and their ultrahigh pressure origin[J].Acta Geologica Sinica,2005(11)
[36]
Bai Wenji ;Shi Nicheng ;Fang Qingsong,Luobusaite: A New Mineral,Acta Geologica Sinica?,2006, 80(5).
[37]
BAI Wenji;YANG Jingsui;FANG Qingsong;REN Yufeng YAN Binggang RONG He.A Study on Os-Ir-Ru Alloy and Boninitic Inclusion in the Luobnsa Ophiolite,Tibet[J].Acta Geologica Sinica,2005(06)
[38]
BAI Wenji;YANG Jingsui;SHI Nicheng;FANG Qingsong DAI Mingqnan XIONG Ming YAN Binggang.A discovery of ultrahigh pressure minerals-Wustite and Native Iron from the mantie ophiolite,in Luobusa,Tibet[J].Geological Review,2002(02)
[39]
BAI Wenji;ROBINSION Paul T;FANG Qingsong;YANG Jingsui,YAN Binggang,ZHANG Zhongming,HU Xuefeng,ZHOU Meifu,The PGE and Base-metal alloys in the podiform chromitites of the Laobusa ophiolite,Southern Tiber,Canadian Mineralogist,2000.
[40]
ARM S;YURIMOTO H,Possible sub-are origi.of podiform chromitites,Island Arc,1995.
ZHOU S;MO M X;MAHONEY J J;ZHANG S Q GUO T J ZHAO Z D,Geochronolagy and Nd and Pb isotope chracteristics of gabbro dikes in the Luobnsa ophiolite,Tibet,Chinese Science Bulletin,2003.
[47]
STOCKMAN H W;HLAVA P F,Platinum-group minerals in Alpine chromitites from southwestern Orogen,Economic Geography,1984.
[48]
KNITTLE E;JEANLOZ R,Simulating the core-mantle boundary:An experimental study of high-pressure reactions between silicates and liquid iron,Geophys,Research Letters,1989.
[49]
KATO T;KUMAZAWA M,Garnet phase of MgSiO3 filling the pyrexene-ilmenite gap at very high temperature,Nature,1985.
[50]
CHEN M;SHU J;XIE X;MAO H,Natural CaTi2O4-structured FeCr2 O4 polymorph in the Suizhou meteorite and its significance in mantle mineralogy,Geochimica et Cosmochimica Acta,2007(20).
[51]
BAI Wenji;PAUL T R;FANG Qingsong;YANG Jingsui YAN Binggang ZHANG Zhongraing HU Xufeng ZHOU Meifu.Chemical compositions of alloys from pediform chromitites in the Luobusa ophiolite,Tibet[J].Acta Geologica Sinica,2006(05)
[52]
王恒升;白文吉;王炳熙,中国铬铁矿床及成因,北京:科学出版社,1983.
[53]
ZHANG J;LI B;UUSUMI W;LIEBERMANN R C,In situ X-ray observations of the cceaitestishovite transition:reversed phase boundary and kinetics,Physics and Chemistry of Minerals,1996.
[54]
ZHANG Hanyong;BA Dengzhu;GUO Tieying,Study of Luobusa Chromite Deposit in Qusong County,Tibet,拉萨:西藏人民出版社,1996.
[55]
Yang, JS ;Dobrzhinetskaya, L ;Bai, WJ ;Fang, QS ;Rolbinson, PT ;Zhang, J ;Green, HW,Diamond- and coesite-bearing chromitites from the Luobusa ophiolite, Tibet,Geology?,2007, 35(10).
[56]
YANG J S;BAI Wenji;FANG Qingsong,Discovery of diamond and an unusual mineral group from the podfform chromite,Poor Rural Geology in China,2007(05).
[57]
YANG J S;BAli W J;FANG Q S;YAN B G Shi N C Ma Z S DAI M Q XIONG M.Silicon-rutile-an ultrahigh pressure (UHP)mineral from an ophiolite[J].Progress in Natural Science,2008(07)
[58]
YANG Fengying;KANG Zhiqin;LIU Shuchun,A new oetabedral pseudomorph of lizardite and its orgin,Acta Mineralogica Sinica,1981(01).
[59]
Richard Wirth ;Alexander Rocholl,Nanocrystalline diamond from the Earth\'s mantle underneath Hawaii,Earth and Planetary Science Letters?,2003, 211(3-4).
[60]
WANG Xibin;BAO Peisheng;DENG Wanming,Xizang (Tibet)Ophiolite,Tectonic Evolution of the Lithosphere of the Himalayas,北京:地质出版社,1987.
[61]
STACHEL T;HARRIS J W;BREY G P,Rare and unusual minend inclusions in diamonds from Mwadui,Tanzania,Contributions to Mineralogy & Petrology,1998.
[62]
RUDASHEVSKY N S;DMITRENKO G G;MOCHALOV A G,Native metals and carbides in alpine type ultramafics of Koryak Highland,Mineralogicheskii Zhurnal,1987(04).
[63]
ROBINSON P T;BAI W J;MALPAS J;YANG J S,ZHOU M F,FANG Q S,HU X F,CAMERON S,STAUDIGEL H,Ultra-high pressure minerals in the Luobnsa Ophiolite,Tibet,and their tectonic implications,Geological Society Special Publication,2004.
[64]
HEN Y;Fei Y;YANG J;BAI W J,XU Z Q SiO2 Solubility in Rutile at High Pressure and Temperature 2005
[65]
MING L C;Bassett W A,High-pressure transformations in the system of MgSiO3-FeSiO3,Earth and Planetary Science Letters,1975.
[66]
LIU Lingun,Effects of H2O on the phase behaviour of the forsterite2enatatite system at high pressure and temperatures and implications for the Earth,Physics of the Earth and Planetary Interiors,1987.
[67]
HAGGERTY S E;SAUTTER V,Ultredeep (greater than 300 kilometers),ultramafic upper mantle xenoliths,Science,1990.
[68]
EDWARDS S J;PEARCE J A;FREEMAN J,New insights conceming the influence of water during the formation of pediform chromite,Geological Society of America Special Paper,2000.
[69]
CHAO E;STISHOVITE C T,SiO2 a very high pressure new mineral from Meteor Crater,Arizona,Journal of Geophysical Research,1962.
[70]
BASSETT W A;MING L C,Dispmportionation of Fe2SiO4 to 2FeO+SiO2 at pressures up to 250 kbar and temperatures up to 3000 degrees C,Physics of the Earth and Planetary Interiors,1972(1-3).