Wu C L;Dong S W;Guo H P;Guo X Y Gao Q M Liu L G Chen Q L Lei M Wooden J L Mazadab F K and Mattinson C.Zircon SHRIMP U-Pb dating of intermediate-acid intrusive rocks from Shizisha,Tongling and the deep processes of magmatism[J].Acta Petrologica Sinica,2008(08)
[3]
Wu C L;Chen S Y;Shi R D;Hao M Y.Origin and features of the mesozoic intermediate-acid intrusive in the tongling area,Anhui,China[J].Acta Geoscientica Sinica,2003(1)
[4]
Tang Y C;Wu Y C;Chu G Z;Xin F M,Wang Y M,Cao F Y and Chang Y F,Geology of copper gold polymetallic deposits in the along-Changjiang area of Anhui Province,北京:地质出版社,1998.
[5]
Sterner S M;Bodnar R J,Synthetic fluid inclusions V Solubility relations in the system NaCl-KCl-H2O under vapor-saturated conditions,Geochimica et Cosmochimica Acta,1988.
[6]
吴才来;陈松永;史仁灯;郝美英.铜陵中生代中酸性侵入体特征及成因[J].地球学报,2003(01)
[7]
Chang Y F;Liu X G,On stratabound skarn:Example from some deposits of the Lower Yangtze River area in Anhui Province,Mineral Deposits,1983(01).
Zeng P S;Yang Z S;Meng Y F;PeiRF Wang Y B Wang X C Xu W Y Tian S H and Yao X D.Temporal-spatial configuration and mineralization of Yanshanian magmatic fluid systems in tongling ore concentration area,Anhui Province[J].Mineral Deposits,2004(3)
[12]
Wu Y C,On magmatic skarn:A new type of skaru,Geology of Anhui,1992(1).
[13]
Jiang Q S;Han C S;Huang J M.Geological features of the copper-lead-zinc deposit in Yaojialing and its genetic discussion[J].Geologyof Anhui,2005(04)
[14]
Hedenquist J W;Arribas R A;Gonzalez-Urien E,Exploration for epithermal gold deposits[A] In,2000.
[15]
Giggenbach W F,The origin and evolution of fluids in magmatichydrothermal systems,New York:John Wiley and Sons,Inc,1997.
[16]
Einaudi T M;Hedenquist J W;Inan E,Sulfidation state of fluids in active and extinct hydrothermal systems:Transitions from porphyry to epithermal environments,Society of Economic Geologists Special Publication,2003.
[17]
Deng J F;Ye D L;Zhao H L;Tang D P,Deep process of the volcanism and the formation of basins in the Lower Yangtze craton,Wuhan:China University Geosciences Publishing House,1992.
[18]
Chang Y F;Liu X P;Wu Y C,The copper-iron belt of the Middle and Lower reaches of the Yangtze River,北京:地质出版社,1991.
Zuo L Y;Hou Z Q;Song Y C;Meng X J and Yang Z S.A study of the ore-forming fluid in the Lengshuikeng Ag-Pb-Zn porphyry deposit[J].Acta Geoscientica Sinica,2009(05)
[30]
Zhai Y S;Yao S Z;Lin X D;Jin F Q,Zhou X R,Wan T F and Zhou Z G,Metallogenic regularity of iron and copper deposits in the middle and lower valley of the Yangtze River,Mineral Deposits,1992(01).
[31]
Zhai Y S;Yao S Z;Lin X D;Zhou X R,Wan T F,Jin F Q and Zhou Z G,Metallogenic regularity of Fe-Cu (-Au) in the Middle-Lower Reach of the Yangtze River area,北京:地质出版社,1992.
[32]
Brown P E;Lamb W M,P-V-T properties of fluids in the system H2O-CO2-NaCl:New graphical presentations and implications for fluid inclusion studies,Geochimica et Cosmochimica Acta,1989.
[33]
Simmons S F;White N C;John D A,Geological characteristics of epithermal precious and base metal deposits,Economic Geology,2005.
[34]
Sillitoe R H;Hedenquist J W,Linkages between volcanotectonic settings,ore fluid compositions and epithermal precious metal deposits,Society of Economic Geologists Special Publication,2003.
[35]
Liu B;Shen K,Thermodynamics of fluid inclusions,北京:地质出版社,1999.
[36]
Jiang Q S;Zhao Z H;Huang J M.Discovery of the Yaojialing copper-lead-zinc deposit in Nanlin,Anhui,and its significance[J].Geology of China,2008(2)
[37]
Brown P E,FLINCOR:A microcomputer program for the reduction and investigation of fluid-inclusion data,American Mineralogist,1989.
