[1] Barten P B.Possible Role of Organic Matter in the Precipitation of the Mississippi Valley Ores[J].Economic Geology,1967,62(3):371-378.
[2] Richard D T,Willden M,Marde Y,et al.Hydrocarbons Associated with Lead-zinc Ores at Laisvall,Sweden[J].Nature,1975,255:131-133.
[3] Macqueen R W,Powel T G.Organic Geochemistry of the
Pine Point Lead-zinc Ore Field and Region,Northwest Territories,Canada[J].Economic Geology,1983,78(1):1-25.
[4] Giordano T H.A Preliminary Evaluation of Organic Ligands and Metal-organic Complexing in Mississippi Valley-type Ore Solution[J].Economic Geology,1985,80(1):96-106.
[5] Gize A P,Barnes H L.The Organic Geochemistry of Two Mississippi Valley-type Lead-zinc Deposits[J].Economic Geology,1987,82(2):457-470.
[6] Disnar J R,Sureau J F.Organic Matter in Ore Genesis:
Process and Perspectives[J].Organic Geochemistry,1990,16(1/3):577-599.
[7] Sims D B.Relationships of Silica,Barite,Organic Material
and Sulfide Minerals at the Red Dog Zn-Pb-Ag Deposit,Western Brooks Range,Alaska[M].Boulder:Geological Society of America,1992.
[8] Kesler S E,Jones H D,Furman F C,et al.Role of Crude Oil in the Genesis of Mississippi Valley-type Deposits:Evidence from the Cincinnati Arch[J].Geology,1994,22(7):609-612.
[9] Gize A P,Barnes H L.Organic Contributions to Mississippi Valley-type Lead-zinc Genesis[C]∥Fontbote L,Boni M.Sediment-hosted Zn-Pb Ore Deposits.Berlin:Springer-Verlag,1994:13-26.
[10] Sicree A A,Barnes H L.Upper Mississippi Valley District
Ore Fluid Model:the Role of Organic Complexes[J].Ore Geology Reviews,1996,11(1):105-131.
[11] Disnar J R.A Comparision of Mineralization Histries for
Two MVT Deposits,Treves and Malines(Causses Basin,France),Based on the Geochemistry of Associated Organic Matter[J].Ore Geology Reviews,1996,11(1):133-156.
[12] 刘文均,伊海生,温春齐.花垣铅锌矿的形成与古油气藏[C]∥叶连俊.生物有机质成矿作用.北京:海洋出版社,1996:154-167.
[13] Spangenberg J E,Macko S A.Organic Geochemistry of the
San Vicente Zinc-lead District,Eastern Pucara Basin,Peru[J].Chemical Geology,1998,146(1/2):1-23.
[14] Spangenberg J E,Fontbote L,Macko S A.An Evaluation of the Inorganic and Organic Geochemistry of the San Vicente Mississippi Valley-type Zinc-lead District,Central Peru:Implications for Ore Fluid Composition,Mixing Processes and Sulfate Reduction[J].Economic Geology,1999,94(7):1067-1092.
[15] Sass-Gusfkiewicz M,Kwiecinska B.Organic Matter in the
Upper Silesian(Mississippi Valley-type)Deposits,Poland[J].Economic Geology,1999,94(7):981-992.
[16] 薛春纪,陈毓川,杨建民,等.滇西北兰坪铅锌银铜矿田含烃富CO2成矿流体及其地质意义[J].地质学报,2002,76(2):244-253.
[17] 朱弟成,朱利东,林 丽,等.西成矿田泥盆系铅锌矿床中的有机成矿作用[J].地球科学——中国地质大学学报,2003,28(2):201-208.
[18] Southam G,Saunders J A.The Geomicrobiology of Ore Deposit[J].Economic Geology,2005,100(6):1067-1084.
[19] Chi G,Savard M M,Héroux Y.Constraints from Fluid Inclusion Data on the Origin of the Jubilee Carbonate-hosted Zn-Pb Deposit,Cape Breton,Nova Scotia[J].Canadian Mineralogist,1995,33:709-721.
[20] 薛春纪,陈毓川,杨建民,等.金顶铅锌矿床地质-地球化学[J].矿床地质,2002,21(3):270-277.
[21] Xue C J,Chen Y C,Wang D H,et al.Geology and Isotopic Composition of Helium,Neon,Xenon and Metallogenic Age of the Jinding and Baiyangping Ore Deposits,Northwest Yunnan,China Series[J].Science in China Series D:Earth Sciences,2003,46(8):789-800.
[22] Xue C J,Zeng R,Liu S W,et al.Geologic,Fluid Inclusion and Isotopic Characteristics of the Jinding Zn-Pb Deposit,Western Yunnan,South China:a Review[J].Ore Geology Reviews,2007,31(1/4):337-359.
[23] Kyle J K,Li N.Jinding:a Giant Tertiary Sandstone-hosted Zn-Pb Deposit,Yunnan,China[J].SEG Newsletter,2002,50:8-16.
[24] 白嘉芬,王长怀,纳荣仙.云南金顶铅锌矿床地质特征及成因初探[J].矿床地质,1985,4(1):1-9.
[25] 高广立.论金顶铅锌矿床的地质问题[J].地球科学——中国地质大学学报,1989,14(5):468-475.
[26] 吴淦国,吴习东.云南金顶铅锌矿床构造演化及矿化富集规律初探[J].地球科学——中国地质大学学报,1989,14(5):477-486.
[27] 赵兴元.云南金顶铅锌矿床成因研究[J].地球科学——中国地质大学学报,1989,14(5):523-530.
[28] 胡明安.试论岩溶型铅锌矿床的成矿作用及其特点——以云南金顶矿床为例[J].地球科学——中国地质大学学报,1989,14(5):531-538.
[29] 尹汉辉,范蔚茗,林 舸.云南兰坪—思茅地洼盆地演化的深部因素及幔-壳复合成矿作用[J].大地构造与成矿学,1990,14(2):113-124.
[30] 王京彬,李朝阳.金顶超大型铅锌矿床REE地球化学研究[J].地球化学,1991,19(4):359-365.
[31] 胡明安.有机质的热液成熟作用在云南金顶铅锌矿床形成过程中的意义[J].地球科学——中国地质大学学报,1989,14(5):503-512.
[32] 王大锐,张 抗.云南地区新生代盆地含油气性[M].北京:
地质出版社,2003.
[33] 常象春,张金亮.金顶铅锌矿区中原油地化特征及其意义[J].特种油气藏,2003,10(5):15-19.
[34] 薛春纪,高永宝,曾 荣,等.滇西北兰坪盆地金顶超大型矿床有机岩相学和地球化学[J].岩石学报,2007,23(11):2889-2900.
[35] 高永宝,薛春纪,曾 荣.滇西北兰坪金顶铅锌矿床有机物质地球化学[J].地球化学,2008,37(3):223-232.
[36] Xue C J,Liu S W,Chen Y C,et al.Giant Mineral Deposits and Their Geodynamic Setting in the Lanping Basin,Yunnan,China[J].Acta Geologica Sinica,2004,78(2):1-7.
[37] 云南省地质矿产局第三地质大队.云南省兰坪县金顶铅锌矿详细勘探地质报告[R].昆明:云南省地质矿产局,1989.
[38] 付修根,林 丽,朱利东.金顶铅锌矿床含矿层沉积环境及成矿条件分析[J].成都理工大学学报:自然科学版,2005,32(5):447-452.
[39] 薛春纪,Chi G X,陈毓川,等.西南三江兰坪盆地大规模成矿的流体动力学过程——流体包裹体和盆地流体模拟证据[J].地学前缘,2007,14(5):147-157.
[40] Chi G X,Xue C J,Lai J Q,et al.Sand Injection and Liquefaction Structures in the Jinding Zn-Pb Deposit,Yunnan,China:Indicators of an Overpressured Fluid System and Implications for Mineralization[J].Economic Geology,2007,102(4):739-743.
[41] 曾 荣,薛春纪,刘淑文,等.金顶超大型铅锌矿床成矿条件分析[J].地球科学与环境学报,2005,27(2):21-25.