Chen Nansheng, Yang Xiuzhen. 1987. Studies of Lizhe molybdenum ore deposit ofsedimentary-magmatic hydropneumatic origin,Lizhe, Zhejiang province. Geochemica, 1987,(3):208~214 (in Chinese with English abstract).
[2]
Chen N, Yang X, Liu D, Xiao X, Fan D L, Wang L. 1990. LowerCambrian rocks seriesand associated stratiform deposits in southern China. Chinese Journal of Geochemistry,8:244~255.
[3]
Coveney R M Jr, Chen N. 1991. Ni-Mo-PGE-Au-rich ores in Chinese black shales andspeculations on possible analogues in the United States. Mineralium Deposita, 26 : 83~88.
[4]
Coveney R M Jr, Gra uch R I. Murowchick J B. 1994. Metal, phosphate, and stonecoal in the Proterozoic and Cambrian of China:The geological setting of preciousmetal-bearing Ni-Mo ore beds.Society of Economic Geologists Newsletter, 18(1): 6~11.
[5]
Creaser R A, Papanastassiou D A, Wasserburg G J. 1991. Negative thermal ion massspectrometry of osmium, rhenium, and iridium.Geochimica et Cosmochimica Acta, 55:397~401.
[6]
Fan Delian, Yang Xiuzhen, Wang Yufang, Chen Nansheng. 1973.Petrological andgeochemical characteristics of a nikel-molybdenum-multe-element-bearing Lower Cambrianblack shale from a certain district in South China. Geochemica, (3): 143~163 (in Chinesewith English abstract).
[7]
Fouquet Y, Von Stackelberg U, Herzig P. 1990. High-temperature polymetallicsulfide deposits in back arc environment: Lau basin SW Pacific. American Association ofPetroleum Geologists Bulletin, 74 :973.
[8]
Grauch R I, Coveney R M Jr, Murowchick J B. 1992. Black shales,continental riftsand Ni-Mo-(PGE-Au) deposits. GSA Annual MTG. Abstrs with Ptogr., 24, A992.
[9]
Holland H D. 1979. Metals in black shales--a reassessment. Economic Geology,74:1676~1680.
[10]
Horan M F, Morgan J W, Gra uch R I, Coveney R M Jr, Murowchick J B, Hulbert L J.1994. Rhenium and osmium isotopes in black shales and Ni-Mo-PGE-rich sulfide layers, YukonTerritory,Canada, and Hunan and Guizhou provinces, China. Geochimica et Cosmochimica Acta,58:257~265.
[11]
Huang Jiqing, Ren Jishun, Jiang Chunfa, Zhang Zhengkun, Qin Deyu. 1980. Tectonicsof China and its evolutions. Beijing: Sciences Press, 1~124 (in Chinese).
[12]
Keays R R, Nickel E H, Groves D I, McGoldrick P J. 1982. Iridium and palladium asdiscriminants of volcanic-exhalative, hydrothermal, and magmatic nikel sulfidemineralization. Economic Geology, 77:1535~1547.
[13]
Kingston-Tivey M. 1995. The influence of hydrothermal fluid compostion andadvection rates on back on black smoker chimney mineralogy: insights from modelingtransport and reaction. Geochemica et Cosmochimica Acta, 58: 257~265.
[14]
Landing E, Bowring S A, Davidek K L, Westrop S R, Geyer G,Heldmaier W. 1998.Duration of the Early Cambrian: U-Pb ages of volcanic ashes from Avalon and Gondwana. Can.J. Earth SCi.35:329~338.
[15]
Lott D A, Coveney R M Jr, Murowchick J B, Grauch R I. 1999.Sedimentary exhalativenickel-molybdenum ores in South China.Economic Geology, 94:1051~ 1066.
[16]
Mao Jingwen, Zhang Zongqing, Dong Baolin. 1990. New Sm - Nd isotopic chronology ofSibao Groupin southern margin of Yangtze massif. Geological Review, 36 : 264~268 (inChinese with English abstract).
[17]
Naldrett A J, Innes D G, Sows J, Gorton M P. 1982. Compositional variations withand between five Sudbury ore deposits. Economic Geology, 77:1519~1534.
[18]
Rowell W F, Edgar A D. 1986. Platinum-group element mineralization in ahydrothermal Cu-Ni sulfide occurrence, Rathbun Lake,northeastern Ontario. EconomicGeology, 81:1272~1277.
[19]
Zeng Mingguo. 1998. Geological characteristics of the Huangjiawan Mo-Ni depositand its development in the future. Guizhou Geology, 15:305~310 (in Chinese).
[20]
Banks D A, Russell M J. 1992. Fluidmixing during ore deposition at the Tynagh base-metal deposit, Ireland. European Journalof Mineralogy, 4: 921~ 931.
[21]
Barnes S J, Boyd R, Korneliusson A, Nilsson L P, Ofetn M, Pedersen B B, Robins B.1988. The use of mantle ratios in discriminating between the effects of partial melting,crystal fractionation and sulfide segregation on platinum-group elements, gold, nickel andcopper: examples from Norway. In: Prichard H M, et al. , ed.Geo-Platinum 87. London:Elsevier, 113~143.
[22]
Bowring S A, Grotzinger J P, Isachsen C E, Knoll A H, Pelechaty S M, Kolosov P.1993. Calibrating rates of Early Cambrian evolution. Science, 262, 1293~1298.
[23]
Charlou J L, Donval J P, Caprais M P. 1990. Hydrothermal activity in the Lau backarc basins: Plumes and hot fluids chemistry.American Association of Petroleum GeologistsBulletin, 74:63.
[24]
Chen Nansheng, Ynag Xiuzhen, Liu Dehan, Xiao Xuejun, Fan Delian, Wang Lianfang.1982. Lower Cambrian lack argillaceous and arenaceous rock series in South China and itsassociated stratiform deposits. Mineral Deposits, 1 (2): 39~ 51 (in Chinese with Englishabstract).
[25]
Coveney R M Jr, Murowchick J B, Grauch R I, Michael D, Glascock D, Denison J D.1992. Gold and platinum in shales with evidence against extraterrestrial sources ofmetals. Chemical Geology, 99:101~114.
[26]
Dong Baolin. 1990. Sibao Group and its relationship to metallogeny.GuangxiGeology, (3):53~58 (in Chinese).
[27]
Fan Delian. 1983. Polyelements in the Lower Cambrian black shale series insouthern China. In: Augustithis S S, ed. The Significance of Trace Metals in SolvingPetrogenetic Problems and Controversies. Athens: Theophrastus Publications S A, 447~474.
[28]
Fan Delian, Yang Ruiying, Huang Zhongxiang. 1984. The Lower Cambrian black shaleseries and iridium anomaly in south China.In: Academia Sinica, Developments in Geoscience,Contributions to 27th IGC, Moscow. 215~224.
[29]
Ganapathy R. 1980. A major meteorite impact on the earth anomalies on the earth 65million years ago : Evidence from the CretaceousTertiary boundary clay. Sciences, 209:921~923.
[30]
Hauri E H, Hart S R. 1997. Rhenium abundances and systematics in oceanic basalts.Chemical Geology, 139 :185~205.
[31]
Hsu K J, Sun Shu, Chen Haihong, Pen Haipo, Sengo A M C. 1988.Mesozoic overthrustsin south China. Geology, 16:418~421.
[32]
Li Shengrong, Gao Zhenmin. 2000. Tracing source for noble metals in the LowerCambrian black shale in Hunan and Guizhou provinces.Sciences of China (Series D), 30:169~174(in Chinese).
[33]
Lowell R P, Rona P A, et al. 1995. Seafloor hydrothermal systems.Journal ofGeophysical Research, 100:327~352.
[34]
McAallum M E, Loucks R R, Carlson R R, Cooley E F, Doerge T A.1976. Platinummetals associated with hydrothermal copper ores of the New Rambler Mine, Medicine BowMountains, Wyoming.Economic Geology, 71:1429~1450.
[35]
Murowchick J B, Coveney R M Jr, Grauch R. 1994. Cyclic variations of sulfurisotopes in Cambrian stratabound Ni-Mo-(PGE-Au) ores of southern China. Geochimica etCosmochimica Acta, 58:1813~1823.
[36]
Ren Jishun. 1991. On the basic characteristics of lithosp herical tectonic ofChina. China Regional Geology, (2): 289~293 (in Chinese with English abstract).
[37]
Smoliar M I, Walker R J, Morgan J W. 1996. Re-Os ages of group Ⅱ A, Ⅲ A, Ⅳ Aand Ⅵ B iron meteorites. Sciences, 271: 1099~1102.
[38]
Volkening J, Walczyk T, Heumann K G. 1991. Osmium isotope ratio determinations bynegative thermal ion mass spectrometry. Int.J. Mass Spect. Ion Proc. , 105:147~159.
[39]
Wang Denghong,Chu Yingshi, Lu Fuxun, Lu Zhi'an, Tang Zhixin.2000. The origin ofthe Cu-Ni-PGE orebody in Ynagliuping,Sichuan province, and the significance of itsdiscovery. Acta Geologics Sinica, 21:260~265 (in Chinese with English abstract).Yang K,Scott S D. 1996. Possible contribution of a metal-rich magmatic fluid to a sea-floorhydrothermal system. Nature, 383:420~423.
[40]
Zhang Guangdi, Mao Jingwen, Xiong Qunyao. 2001. The present situation andprospects of platinum metals resources in China. Acta geoscientia Sinica, 22(2):107~110(in Chinese with English abstract).
[41]
Zimmerman R K, Kesler S E. 1981. Fluid inclusion evidence for solution mixing,Sweetwater (Mississippi Valley-type) district, Tennessee. Economic Geology, 76:134~142.