Xue C J,Ma G L,Wei H M and Zeng Z R.1996.REE geochemistry of main types of hydrothermal sedimentary rocks in South Qinling[J].Journal of Xi\'an College of Geology,18(3):21～28 (in Chinese with English abstract).
[2]
Xue C J,Ji J S,Zhang L C,Lu D R,Liu H S and Li Q L.1997.The Jingtieshan submarine exhalative-sedimentary iron-copper deposit in North Qilian Mountain[J].Mineral Deposits,16(1):21～30 (in Chinese with English abstract).
[3]
Zhang D Q,Feng C Y,LI D X,Xu W Y,Yan S H,She H Q,Dong Y J and Cui Y H.2001.Orogenic gold deposit in the north Qaidam and east Kunlun orogen,west China[J].Mineral Deposits,20(2):137～146 (in Chinese with English abstract).
[4]
Zhang D Q,Wang Y,Feng C Y,Li D X,Yan S H,Cui Y H.2002.Geology and geochemistry of Tuolugou exhalative-sedimentary Co-Au deposit,Qinghai Province[J].Mineral Deposits,21(3):213～222 (in Chinese with English abstract).
[5]
Zhang D Q,Dang X Y,She H Q,Li D X,Feng C Y and Li J W.2005.Ar-Ar dating of orogenic gold deposit in northern margin of Qaidam and East Kunlun Mountains and its geological significance[J].Mineral Deposits,24(2):87～98 (in Chinese with English abstract).
[6]
Zhu H P,Sun F Y,Li B L,Chen G H and Chi X G.2004.Study on the geological characteristics of Tuolugou Co deposit and ore prospecting,Qinghai Province[J].Contributions to Geology and Mineral Resource Research,19(3):147～152 (in Chinese with English abstract).
Annels A E,Vaughan D J and Craig J R.1983.Conditions of ore mineral formation in certain Zambian copper belt deposits with special reference to the role of cobalt[J].Mineralium Deposita,18:71～88.
[23]
Bhatia M R.1983.Plate tectonics and geochemical composition of sandstones[J].Journal of Geology,91:611～627.
[24]
Bhatia M R and Crook K A W.1986.Trace element characteristics of graywackes and tectonic setting discrimination of sedimentary basin[J].Contrib.Mineral Petrol.,92:181～193.
[25]
Clayton R N.1972.Oxygen isotope exchange between quartz and water[J].J.Geophys.Res.,77:3057～3607.
[26]
Crerar D A,Namson J and Chyi M S.1982.Manganiferous chert of the Franciscan assemblage:Ⅰ.General geology ancient and modern analogues and implications for hydrothermal convection at oceanic spreading centers[J].Economic Geology,77(3):519～540.
[27]
Feng C Y,Zhang D Q,Wang F C,Li D X and She H Q.2004.Geochemical characteristics of ore-forming fluids from the orogenic Au (and Sb) deposits in the eastern Kunlun area,Qinghai Province[J].Acta Petrologica Sinica,20(4):949～960 (in Chinese with English abstract).
[28]
Feng C Y,Zhang D Q,Qu W J,Du A D,Li D X and She H Q.2006.Re-Os isotopic dating of pyrite in the Tuolugou SEDEX cobalt (gold) deposit,Gulmud city,Qinghai Province,China[J].Acta Geologica Sinica,80(4):571～576 (in Chinese with English abstract).
[29]
German C R,Hergt J and PaFFer M R.1999.Geochemistry of a hydrothermal sediment core from the OBS vent-field,21°N East Pacific Rise[J].Chem.Geol.,155:65～75.
[30]
Goodfellow W D,Lydon J W and Turner R J W.1993.Geology and genesis of stratiform sediment-hosted (Sedex) zinc-lead-silver sulphide deposits[A].In:Kirkham R V,Sinclair W D and Thorpe R I,ed.Mineral deposit modeling[C].Geological Association of Canada,Special Paper 40.201～251.
[31]
Gu X X,Schulz O,Vavtar F,Liu J M and Zheng M H.2003.Ore fabric characteristics of Woxi W-Sb-Au deposit in Hunan and their genetic significance[J].Mineral Deposits,22(2):107～120 (in Chinese with English abstract).
[32]
Han F and Hutchinson R W.1989.Evidence for hydrothermal exhalative sedimentary origin of the Dachang tin-polymetallic deposit:Geochemistry of rare earth elements and trace elements of the host rocks[J].Mineral Deposits,8(3):33～42 (in Chinese with English abstract).
[33]
Han F and Hutchinson R W.1990.Evidence for exhalative origin of the Dachang tin-polymetallic sulfide deposits:Their geological and geochemical characteristics[J].Mineral Deposits,9(4):309～324 (in Chinese with English abstract).
[34]
Leblanc M and Billaud P.1982.Cobalt arsenide orebodies related to an upper Proterozoic ophiolite:Bou Azzer (Morocco)[J].Economic Geology,77:162～175.
[35]
Li H M,Shen Y C and Hu Z G.2000.Geological characteristics of the Tuolugou cobalt (gold) deposit in East Kunlun,Qinghai Province[J].Bulletin of Mineralogy,Petrology and Geochemistry,19(4):321～322 (in Chinese).
[36]
Lott D A,Coveney R M Jr,Murowchick J B and Grauch R I.1999.Sedimentary exhalative nickel-molybdenum ores in South China[J].Econ.Geol.,94:1051～1066.
[37]
Lottermoser B G.1989.Rare earth element study of exhalites within the Willyama Supergroup,Broken Hill Block,Australia[J].Mineralium Deposita,24:92～99.
[38]
Maynard J B,Vallon R and Yu H.1982.Composition of modern deep sea sands from arc-related basins[J].Geological Society of London,Special Publication,10:551～561.
[39]
Mills R A and Elderfield H.1995.Rare earth element geochemistry of hydrothermal deposits from the active TAG Mound,26°N Mid-Atlantic Ridge[J].Geochim.Cosmochin.Acta,59(17):3511～3524.
[40]
Modreski P J.1985.Stratabound cobalt-copper deposits in the Middle Proterozoic Yellowjacket Formation in and near the Challis Quadrangle,Idaho[J].U.S.Geological Survey Bullettin,1658A-S:203～221.
[41]
Murray R W,Brink M R B and Gerlach D C.1990.Rare earth elements as indicators of different marine depositional environments in chert and shale[J].Geology,18(3):268～271.
[42]
更多...
[43]
Murray R W.1994.Chemical Criteria to identify the depositional environment of chert:General principles and applications.Sedimentary Geology,90:213～232.
[44]
Nash J T and Hahn G A.1989.Stratabound Co-Cu deposits and mafic volcaniclastic rocks in the Blackbird mining district,Lemhi County,Idaho[J].Geological Society of Canada,Special Paper 36,339～356.
[45]
Nash J T and Connor J.J.1993.Iron and chlorine as guides to stratiform Cu-Co-Au deposits,Idaho cobalt belt,U.S.A[J].Mineralium Deposita,28:99～106.
Pan Y M and Therens C.2000.The Werner Lake Co-Cu-Au deposit of the English River Subprovince,Ontario,Canada:Evidence for an exhalative origin and effects of granulite facies metamorphism[J].Economic Geology,95:1635～1656.
[48]
Parr J M.1992.Rare-earth element distribution in exhalites associated with Broken Hill-type mineralization at the pinnacles deposit,New South Wales,Australia[J].Chem.Geol.,100:73～91.
[49]
Pearce J A.1983.Role of the sub-continental lithosphere in magma genesis at active continental margin[A].In:Hawkesworth C J and Norry M J,ed.Continental basalts and mantle xenoliths[C].Nantwich,U.K:Shiva Publishing Ltd.230～249.
[50]
Roser B P and Korsch R J.1986.Determination of tectonic setting of sandstone-mudstone suites using SiO2 content and K2O/Na2O ratios[J].Journal of Geology,94:635～650.
[51]
Sangster D F and Hillary E M.1998.Sedex lead-zinc deposits:proposed sub-types and their characteristics[J].Exploration and Mining Geology,7:341～357.
[52]
Sheppard S M F.1986.Characterization and isotope variations in natural waters[J].Reviews in Mineralogy,16:165～183.
[53]
Sweeney M,Turner P and Vaughan D J.1986.Stable isotope and geochemical studies in the role of early diagenesis in ore formation,Konkola basin,Zambian copper belt[J].Economic Geology,81:1838～1852.
[54]
Tang J,Wang F M,Xu H Y,Li S P and Zhang L.2004.Characteristics of ore-hosted strata and ore-controlling structure of Co-Au mineral deposit in Tuolugou area,Qinghai[J].Northwestern Geology,37(1):86～96 (in Chinese with English abstract).
[55]
Taylor H.P.1979.Oxygen and hydrogen isotope relationships in hydrothermal mineral deposits[A].In:Barnes H L,ed.Geochemistry of hydrothermal ore deposits[C].New York:Wiley Interscience.611～631.
[56]
Taylor S R and McLennan S M.1985.The Continental Crust:Its composition and evolution[M].Oxford:Blackwell.1～312.
[57]
Wei J Y and Wang G Y.1988.Isotope geochemistry[M].Beijing:Geol.Pub.House.1～149 (in Chinese)
[58]
Xie G Q,Hu R Z,Fang W X and Xi L.2002.Evidence for geology and geochemistry of hydrothermal exhalative genesis from Mojiang gold deposit,Yunnan[J].Acta Sedimentologica Sinica,20(3):387～393 (in Chinese with English abstract).
