XIAO Hua-yun,LIU Cong-qiang,HUANG Jiu-long . NFORMATION OF OLD MANTLE FROM INCLUSIONS IN DIAMONDS[J]. Advances in Earth Science, 2001 , 16(2) : 244 -250 . DOI: 10.11867/j.issn.1001-8166.2001.02.0244

[1]  Richardson S H, Gurney J J, Erlank A J,et al. Origin of diamonds in old enriched mantle[J]. Nature, 1984, 310: 198~202.
[2]  Mitchell R H. Kimberlites and lamproites primary sources of diamond[J]. Geoscience Canada, 1991, 18: 1~16.
[3]  Lang A R. Internal structure[A]. In: Field J E, ed. The Properties of Diamond[C], London: Academic Press, 1979.425~426.
[4]  Bulanova G P. The formation of diamond[J]. J Geochem Explor, 1995, 53: 1~23.
[5]  Bulanova G P, Griffin W L, Ryan C G. Nucleation environment of diamonds from Yakutian kimberlites [J]. Mineral Magazine, 1998, 62: 409~419.
[6]  Bulanova G P, Griffin.W L, Ryan C G,et al. Trace elements in sulfide inclusions from Yakutian diamonds[J]. Contri Mineral Petrol, 1996, 124: 111~125.
[7]  Lambrecht W R L, Lee C H, Segall B,et al. Diamond nucleation by hydrogenation of the edges of graphitic precursors[J]. Nature, 1993, 364: 607~610.
[8]  Milledge H J, Woods P A, Taylor W R,et al. Cathodoluminescence and infrared studies of russian diamonds[A]. In:Abstr IAVCEI General Assembly [C]. Canberra, 1993.pp74.
[9]  Griffin W L, Gurney J J, Ryan C G. Variations in trapping temperatures and trace elements in peridotite-suite inclusions from African diamonds: evidence for two inclusion suites, and implications for lithospere stratigraphy[J]. Contrib Mineral Petrol, 1992, 110: 1~15.
[10]  Griffin W L, Sobolev N V, Ryan C G,et al. Trace elements in garnets and chromites: Diamond formation in the Siberian lithospere[J]. Lithos, 1993, 29: 235~256.
[11]  Cheng F,Guo J G,Chen J C,et al. Potassic salt inclusions found in diamonds[J]. Chinese Science Bulletin, 1992, 37(10): 921~923(in Chinese).
[12]  Cheng F,Guo J G,Wang S X,et al. NaCl inclusions found in diamonds[J]. Chinese Science Bulletin, 1992, 37(16): 1 489~1 491 (in Chinese).
[13]  Leng I, Guo W, Friendman I. Natural occurrence of silicon carbide in a diamondiferous kimberlite from Fuxian[J]. Nature, 1991, 346: 352~354.
[14]  Zhao L, Lu F X, Zheng J P,et al. Natural silver and silvercontaining iron-gold alloy inclusions found in diamonds the first time[J]. Chinese Science Bulletin, 1995, 40(12): 1 114~1 115(in Chinese).
[15]  Ellis D J, Green D H An experimental study of the effect of Ca upon garnet-clinopyroxene Fe-Mg exchange equilibria[J].Contrib Mineral Petrol, 1979, 71: 13~22.
[16]  Griffin W L, Jaques A L, Sie S H,et al. Conditions of diamond growth: a proton microprobe study of inclusions in West Australian diamonds [J]. Contrib Mineral Petrol,1988, 99: 143~158.
[17]  Griffin W L, Sobolev N V, Ryan C G,et al. Trace elements in garnets and chromites: diamond formation in the Siberian lithosphere[J]. Lithos, 1993, 29: 236~257.
[18]  O' Neill HSt C, Wall V G. The olivine-orthopyrexene-spinel oxygen geobarneter, the nickle precipitation curve, and oxygen fugacity of the Earth' s upper mantle[J]. J Petrol, 1987,28: 1 169~1 191.
[19]  Jarikov V A, Ishbulatov R A, Chudinovskih L T. The eclogitic barrier and clinopyroxenes of high pressure[J]. Geol Geophys, 1984, 12: 54.
[20]  Brey G P, Nickel K G, Kogarko L. Garnet pyroxene equilibrium in system Cao-MgO-Al2O3-SiO2( CMAS ), and prospects for simplified (T-independent) lherzolite barometry and eclogite-barmeter[J]. Contrib Mineral Petrol, 1986, 92:448~453.
[21]  Jaques A L, Haggerty S E, Lucas H,et al. Mineralogy and petrology of the Argyle (AK1) lamproite pipe, Western Australia. Kimberlites and related rocks, vol 1: Their composition, occurrence, origin and emplacement[J]. Geol Soc Aust Spec Publ, 1989, 14: 153~169.
[22]  Kesson S E, Ringwood A E. Slab-mantle interactions 2. The formation of diamonds[J]. Chem Geol, 1989, 78: 97~118.
[23]  Liu L-g, Mernagh T P, Jaques A L. A mineralogical Raman spectroscopy study on eclogitic garnet inclusions in diamonds from Argyle[J]. Contrib Mineral Petrol, 1990, 105: 154~161.
[24]  Liu L-g. Genesis of diamonds in the lower mantle[J]. Contrib Mineral Petrol, 1999, 134: 170~173.
[25]  Moore R O, Gurney J J. Pyroxene solid solution in garnets included in diamond[J]. Nature, 1985, 318: 553~555.
[26]  Irifune T, Sekine T, Ringwood A E,et al. The eclogite-garnet transformation at high pressure and some geophysical implications[J]. Earth Planet Sci Lett, 1986, 77: 245~256.
[27]  Boyd F R, Gurney J J, Richardson S H. Evidence for a 150~200 km thick, Archaean lithosphere from diamond inclusion thermobarometry[J]. Nature, 1985, 315: 387~389.
[28]  Moore R O, Gurney J J, Griffin W L,et al. Ultra-high pressure garnet inclusions in Monastery diamonds: trace element abundance patterns and conditions of origin[J]. Eur J Mineral, 1991, 3: 213~230.
[29]  Sunagawa I. Characteristics of crystal growth in nature as seen from the morphology of mineral crystals[J]. Bull Mineral, 1981, 104: 81~87.
[30]  Sunagawa I. Growths of crystals in nature[A]. In: Sunagawa I.Materials Science of the Earth' s Interior[C]. Tokyo:Terrapub, 1984.61~103.
[31]  Sunagawa, I. Morphology of natural and synthetic diamond crystals[A]. In: Sunagawa l,ed. Materials Science of the Earth' s Interior[C]. Tokyo: Terrapub,1984.303~331.
[32]  Arima M, Nakayama K, Yamaoka S,et al. Crystallization of diamond from a silicate melt of kimberlite composition in high-pressure and high-temperature[J]. Geology, 1993, 21:968~970.
[33]  Saxena S K. Oxidation state of the mantle[J]. Geochim Cosmochim Acta, 1989, 53: 89~95.
[34]  Chepurov A I. On the role of sulfide melt in the process of diamond origin[J]. Geol Geophys, 1988, 8: 110~124.
[35]  Bulanova G P, Spetsius Z V, Leskova N V. Sulfides in Diamond Growth and Mantle Xenoliths from Kimberlite Pipes of Yakutiya[M]. Novosibirsk: Nauka, 1990. pp118.
[36]  Navon O, Hutcheon I D, Rossman G R,et al. Mantle-derived fluids in diamond micro-inclusions[J]. Nature, 1988,335: 784~789.
[37]  Schrauder M, Navon O. Hydrous and carbonatitic mantle fluids in fibrous diamonds from Jwaneng, Botswana [J].Geochim Cosmochim Acta, 1994, 58: 761~771.
[38]  Schrauder M, Koeberl C, Navon O. Trace element analyses of fluid-bearing diamonds from Jwaneng, Botswana [J].Geochim CosmochimActa, 1996, 60: 4 711~4 724.
[39]  Roedder E. Fluid inclusions[J]. Reviews in Mineralogy,1984, 12: 1~664.
[40]  Richardson S H, Gurney J J, Erlank A J,et al. Origin of diamond in old enriched mantle[J]. Nature, 1984, 310: 198~202.
[41]  Navon O. High internal pressures in diamond fluid inclusions determined by infrared absorption[J]. Nature, 1991, 353:746~748.
[42]  Guthrie Jr G D, Veblen D R, Navon O,et al. Submicrometer fluid inclusions in turbid-diamond coats[J]. Earth Planet Sci Lett, 1991, 105: 1~12.
[43]  Lu F X, Zhao L, Zheng J P. Geochemistry of mantle fluids and asthenosphere, related with kimberlites[A]. In: Du L T, ed. Geochemistry of Mantle Fluids and Asthenosphere(asthenoliths). Beijing: Geological Publishing House.1996.97~153(in Chinese).
[44]  Chrenko R M, McDonald R S, Darrow K A. Infra-red spectra of diamond coat[J]. Nature, 1967, 213: 474~476.
[45]  Zheng J P, Lu F X, Guo H,et al. Studies of fluid inclusions in diamonds[J]. Chinese Science Bulletin, 1994, 39(3): 253~256.