Auge T. 1988. Platinum group minerals in the Tiebaghi and Veurinos ophiolite complex: genetic implications. Canadian Mineralogist,26: 177~192.
[5]
Bai Wenji, Zhou Meifu, Robinson P T, et al. 2000. Origin of podiform chromitite, diamond and their associated minerals at Luobusa, Tibet. Beijing: Seismological Publishing House, 1~ 98(in Chinese with English abstract).
[6]
Bai Wenji, Yang Jingsui, Fang Qingsong, et al. 2001. Study on a storehouse of ultrahigh pressure mantle minerals-podiform chromite deposits. Earth Sci. Frontiers 8 (3): 111 ~ 121 (in Chinese with English abstract).
[7]
Bai Wenji, Yang Jingsui, Fang Qingsong, et al. 2004. Chemical compositions of alloys from podiform chromitites in the Luobusa ophiolite, Tibet. Acta Geologica Sinica, 78 (5): 675~682 (in Chinese with English abstract).
[8]
Bird J M. 1979. Origin of Josephinite. Geochemical Journal, 13:41 ~55.
[9]
Bird J M, Bassett W A. 1980. Evidence of a deep mantle history in Terrenstria osmium-iridium ruthenium alloys. Journal of Geophysical Research, 85 (1310): 5461~5470.
[10]
Brenker F E, Meibom A, kobett F. 2003. On the formation of peridotite-derived Os-rich PGE alloys. American Mineralogist,88: 1731~1740.
[11]
Dick H J B, Gillete H. 1976. Josephinite-specimens from the core? A discussion. Earth and Planetary Science Letters, 31: 308~311.
[12]
Dick H J B, Bullen T. 1984. Chromian spinel as a petrogenetic indicator in abyssal and Alpine-type peridotites and spatially associated lavas. Contribution to Mineralogy and Ptrology, 86:54~76.
[13]
Eckstrend O K. 1975. The Dumont serpentinite: a model for control of nickeliferous opaque mineral assemblages by alteration reactions in ultramafic rocks. Economic Geology and the Bulletin of the Society of Economic Geologist, 70: 183~201.
[14]
Falloon T J,Green D H, McCulloch M T. 1989. Petrogenesis of high-Mg and associated lavas from the North Tonga trench. In:Crawford A J,eds. Boninites and Related Rocks. Unaya,Hyman,London, 357~395.
[15]
Finger L W, Hazen R M. 1991. Crystal chemistry of six-coordinated silicon: a key to understanding the Earth\'s deep interior. Acta Crystalloger, B47: 561~580.
[16]
Garuti G, Zaccarini F. 1997. In situ alteration of platinum-group minerals at low temperature: evidence from serpentinized and weathered chromitite of the Vourinos complex. Greece. Canadian Mineralogist, 35: 611 ~ 626.
[17]
Harris D C, Cabri L J. 1991. Nomenclature of platinum group element alloys: review and revision. Canadian Mineralogist, 29: 231 ~237.
[18]
Hazen K M, Downs K T, Finger L W. 1993. Crystal chemistry of ferromagnesian silicate spinels: Evidence for Mg-Si disorder.American Mineralogist, 78: 1320~ 1323.
[19]
Melcher F, Grum W, Simon G, et al. 1997. Petrogenesis of the ophiolitic giant chromite deposits of Kempirsai, Kazakhstan. A study of solid and fluid inclusions in chromite. Jourmal of Petrology, 38:1419 ~ 1458.
[20]
Stockman H W, Hlana P F. 1984. Platinum-group minerals in Alpine chromitites form southweastern Oregon. Economic Geology, 79:491~508.
[21]
Talkington K W, Watkinson D H, Whitaker P T, et al. 1984.Platinum-group minerals and other solid inclusions in chromite of ophiolitic complexes: occurrence and petrological. Tschermaks Mineralogische und Petrographische Mittilungen, 32: 285~301.
[22]
Zhou M F. 1995. Petrogenesis of the podiform chromitite in the Luobusa ophiolites, Southern Tibet. Unpublished PHD thesis,Dalhousie University.
Arai S. 1992. Chemistry of chromian spinel in volcanic rocks as a potential guide to magma chemistry. Mineral Mag. , 56:173 ~184.
[26]
Bai Wenji, Robinson Paul T, Fang Qingsong, et al. 2000. The PGE and base-metal alloys in the podiform chromites of the Luobusa ophiolite, southern Tibet. Canadian Mineralogist, 38:585 ~598.
[27]
Bai Wenji, Yang Jingsui, Fang Qingsong, et al. 2003. An unusual mantle mineral group in ophiolites of Tibet. Geology in China, 30(2): 144~150 (in Chinese with English abstract).
[28]
Ballhaus C. 1998. Origin of podiform chromite deposits by magma mingling. Earth and Planetary Science Letters, 156: 185~193.
[29]
Bird J M, Weathers M S. 1975. Josephinite: specimens from the Earth core? Earth and Planetary Science Letters, 28: 51~64.
[30]
Bird J M, Meibom A, Frei R, Nagler T H. 1999. Osmium and lead isotopes of rare Os-Ir-Ru minerals: derivation from the coremantle boundary region? Earth and Planetary Science Letters,170: 83~92.
[31]
Bohlen S R, Boettecher A L. 1982. The quartz coesite transformation: a pressure determination and effects of other components. Journal of Geophysical Research, 87: 7073~7078.
[32]
Cameron W E. 1985. Petrology and origin of primitive lavas from the Troodos ophiolite. Contrib. Mineral Petrol. ,89: 239~255.
[33]
Chamberlain J A. 1965. Native metals in the Muskov intrusion.Canadian Journal of Earth Sciences, 2: 188~215.
[34]
Crawford A J, Falloon T J, Green D H. 1989. Classification,petrogenesis and tectonic setting of boninites. In: Crawford A J,ed. Boninite and Related Rocks, 1 ~ 49.
[35]
Dick H J B. 1974. Terrestrial nickel-iron from the Josephine peridotite, its geological occurrence, associations and origin.Earth and Planetary Science Letters, 24: 291~ 298.
[36]
Enami M, Zang Q. 1990. Quartz pseudomorphs after coesite in eclogites from Shandong province, east China. American Mineralogist, 75: 381~386.
[37]
Falloon T J, Danyushevsky L V. 2000. Melting of refractory mantle at 1.5, 2 and 2.5 GPa under anhydrous and H2O-undersaturated conditions: Implications for the petrogenesis of high-Ca boninites and the influence of subduction components on mantle melting.Journal of Petrology, 41: 257~283.
[38]
Hirajima T, Ishiwatari A, Cong B, et al. 1990. Coesite from Mengzhong eclogite at Donghai county, northeastern Jiangsu province, China. Mineralogical Magazine, 54: 579~583.
[39]
Jonieson G S. 1905. On the natural iron-nickl alloy awaruite.American Journal of Science, 19: 413.
[40]
Matveev S, Ballhaus C. 2002. Role of water in the origin of podiform chromitite deposits. Earth and Planetary Science Letters, 203:235~243.
[41]
Ramdohr P. 1950. Uher Josephinite, Awarit, Souesite ihrer Eigenschaften. Entstehung und Paragenesis. Mineralogical Magazine, 12: 374.
[42]
Robinson P T, Bai W J, Malpas J, et al. 2004. Ultra-high pressure minerals in the Luobusa ophiobite, Tibet and their tectonic implications. in Aspects of the Tectonic Evolution of China.Geological Society, London, Special Publications, 226:247 ~271.
[43]
Yang Jingsui, Bai Wenji, Fang Qingsong. et al. 2003. Silicon-rutile ultra-high pressure mineral from ophiolits. Progress in Nature Science, 13 (7) :528~531.