Yan J;Chen J F;Yu G.Pb isotopic characteristics of late Mesozoic mafic rocks from the lower Yangtze region:evidence for enriched mantle[J].Geological Journal of China Universities,2003(02)
[10]
Xing F M;Xu X,Basic Characteristics of the Mesozoic Magmatic Rocks along the Yangtze River,Anhui,Geology of Anhui,1995(01).
[11]
Wu G G;Zhang D;Zang W S.Study on Tectonic layering Movement and Layering Mineralization in the Tongling Metallogenic Cluster[J].Science in China (Series D),2003(08)
[12]
Wu C L;Zhou X R;Huang X C,40Ar/39Ar chronology of intrusive rocks from Tongling,Acta Petrologica et Minerologica,1996(04).
[13]
Wei J Y;Wang G Y,Isotopes geochemistry,北京:地质出版社,1988.
[14]
Wedepohl K H,Chemical composition and fractionation of the continental crust,GEOLOGISCHE RUNDSCHAU,1991.
[15]
Taylor H P,Oxygen,hydrogen,and strontium isotope constrains on the origin of granites,Trans Royal Soc Edinb Earth Sci,1988.
[16]
Shen W Z;Ling H F;Li W X,Study on the Nd-Sr isotopic compositions of granitoids in SEChina,Geol J China Uni,1999(01).
[17]
Rudnick R L;Fountain D M,Nature and composition of the continental crust:a lower crust perspective,REVIEWS OF GEOPHYSICS,1995.
[18]
Pei R F;Lv F X;Fan J Z,Metallogenetic series and exploration of the metal deposits in north margin of the North China Massif and its north side,北京:地质出版社,1998.
[19]
Middlemost E A K,Magmas and magmnatic rocks,Longman,Lodon,1985.
[20]
Meissner R;Tanner B,From collision tocollapse:phases of lithospheric evolution as monitored by seismicrecords,Phys Earth Planet Interiors,1993.
[21]
McDonough W F;Sun S S;Ringwood A E,Potassium,rubidium,and cesium in the earth and moon and the evolution of the mantle of the earth,Geochimica et Cosmochimica Acta？ ,1992, 56.
[22]
Mao J W;Zhang Z H;Yu J J,Geodynamic setting of Mesozoic large-scale mineralization in the North China and adjacent areas:implications for highly precise and accurate ages of metal deposits,Science in China (Series D),2003(04).
[23]
Mei Y X;Mao J W;Li J W.Re-Os dating of the molybdeite occurring in stratiform skarn orebody in the Datuanshan Cu ore deposit,Anhui Province,and its geological significance[J].Acta Geoscientica Sinica,2005(04)
[24]
Lu Q T;Hou Z Q;Zhao J H.Complicated crustal structures in the Tongling metallogenic province revealed on the deep seismic reflection profile[J].Science in China (Series D),2003(05)
[25]
Kay R W;Kay S M,Creation and destruction of lower continental crust,Geologische Rundschau？ ,1991, 80.
[26]
Huang X C;Chu G Z,Multistory metallogenic model of the Shizishan orefield in Tongling,Anhui Province,Mineral Deposits,1993(03).
[27]
Hu Shouxi;Zhou Sunzi;Sun Zhiming,On the metallogenic specialization of the middle-acid rocks related to Fe,Cu deposits in the eastern China,Acta Geologica Sinica,1979(04).
[28]
Guo Wenkui,ON the genesis of the Tongguanshan copper deposit,Acta Geologica Sinica,1957(03).
[29]
Gao S;Zhang B R;Luo T C,Chemical composition of the continental crust in the Qinling Orogenic Belt and its adjacent North China and Yangtze cratons,GEOCHIMICA ET COSMOCHIMICA ACTA,1992.
[30]
Faure G,Principles of isotope geology,New York:John Wiley and Sons,Inc,1977.
[31]
Di Y J;Zhao H L;Zhang Y Q,Petrographic evidences for magma mixing in the granitoids from Tongling area,Anhui province,Beijing Geology,2003(01).
[32]
陈江峰;周泰禧;邢凤鸣,长江中下游岩带含铜岩体的Pb、Sr、Nd同位素特征,地球学报,1994.
[33]
常印佛;刘湘培;吴昌言,长江中下游铁铜成矿带,北京:地质出版社,1991.
[34]
Chen J F;Zhou T X;Xing F M,Pb,Sr and Nd isotope characteristics copper-bearing rocks from middle-low area of Yangtze,ACTA GEOSCIENTIA SINICA(IN CHINESE),1994.
[35]
Chen J F;Foland K A;Zhou Taixi,Mesozoic granitoids of the Yangtze foldbelt,China:Isotopic constrains on the magma source,Theophrastus,Athens,1985.
[36]
Chang Y F;Liu X P;Wu Y C,The copper and ore belt in the middle and lower reaches of the Yangtze River,北京:地质出版社,1991.
[37]
Boynton W V,Geochemistry of the rare earth elements:meteorite studies,Elservier,1984.
Liu Y Q;Liu Z L,Isotope geochemistry and genesis of the stratiform copper (iron-sulfer) deposits in T ongling arer,Anhui Province,Bulletin of the Institute of Mineral Deposits,1991(01).
[57]
Liu Y J;Cao L M,Elements geochemistry,北京:地质出版社,1987.
[58]
Den J F;Ye D L;Zhao H L,Volcanism deep internal progresses and basin forrruztion in the lower Reaches of the Yangtze River,武汉:中国地质大学出版社,1992.
Zindler A;Hart S,Chemical geodynamics,Ann Rev,EARTH AND PLANETARY SCIENCE LETTERS,1986.
[62]
Zhou T F;Yue S C.Forming Conditions and Mechanism for the fluid Ore-forming system of the copper,Gold Deposits in the middle and lower Reaches of the Yangtze River area[J].Universitatis Pekinensis(Acta Scientiarum Naturalium),2000(05)
[63]
Zhen Y F;Chen J F,Stable isotopes geochemistry,北京:科学出版社,2002.
[64]
Zhang Q;Wang Y;Liu H T.On the space-time distribution and geodynamic environments of adakites in china annex:controversies over differing opinions for adakites in china[J].Earth Science Frontiers,2003(04)
[65]
Xing F M;Xu X,High-potassium calc-alkaline intrusive rocks in Tonglingarea,Anhui province,Geolchimica,1996(01).
[66]
Wu C L;Wang Z H;Qiao D W.Types of enclaves and their features and origins in intermedite-acid intrusive rocks from Tongling district,Anhui,China[J].Acta Geologica Sinica,2000(01)
[67]
Wei J H;Lin C Q;Tang H F.Metallogeny of gold deposits and evidence of isotopes for the comagmatic evolution of the Yanshanian intrusive rocks in the Wulong area,Eastern Liaoning[J].GEOLOGICAL REVIEW,2003(03)
[68]
Wang Q;Xu J F;Zhao Z H.Petrogenesis of the Mesozoic intrusive rocks in the Tongling Area,Anhui Province,China and constraint to geodynamics process[J].Science in China (Series D),2003(04)
[69]
Wang Y J;Fan Y M;Guo F.Geochemical characteristics of late mesozioc volcanic rocks in the hinterland of north Dabie terrene and their tectonic implications[J].Earth Science Frontiers,2003(04)
[70]
安徽省地质矿产局321地质队,铜陵地区铜金多金属隐伏矿床预测,1995.
[71]
邓晋福;叶德隆;赵海玲,下扬子地区火山作用深部过程与盆地形成,武汉:中国地质大学出版社,1992.
[72]
Stacey J S;Hedlund D C,Lead-isotope compositions of diverse igneous rocks and ore deposits from southwestern NewMexico and their implications for early Proterozoic crustal evolution in the westem United States,GEOLOGICAL SOCIETY OF AMERICA BULLETIN,1983.
[73]
Rickwood P C,Boundary lines within petrologic diagrams which use oxides of major and minor elements,LITHOS,1989.
[74]
Mengel K;Kem H,Evolution of the petrological and seismic Moho-implications for the continental crust-mantle boundary,TerraNova,1992.
[75]
Mao J W;Stein H;Du A D.The Re-Os isotope accurate timing of copper (molybedenum) in the Middle and Lower Yangtze area and its indication for metallogenesis[J].Acta Geological Sinica,2004(01)
[76]
Kutina J;Pei Rongfu;Heyl A V The role of deep lithospheric structure in the genesis and distribution of giant and supergiant concentrations of metals in the crust [J] 2003(1-4)
[77]
Guo Zongsan,Some skarn copper deposits in Lower Yangtze River valley,Acta Geologica Sinica,1957(01).
[78]
Guo Wenkui,On the granitoids and metal mineralization,Regional Geology of China,1982(02).
[79]
Gao S;Jin Z M,Delamination and its geodynamical significance for the crust-mantle evolution,Geological Science and Technology Information,1997(01).
[80]
Alain Dupont ；Jacqueline Vander Auwera ；Christian Pin,Trace element and isotope (Sr, Nd) geochemistry of porphyry- and skarn-mineralising Late Cretaceous intrusions from Banat, western South Carpathians, Romania,Mineralium deposita？,2002, 37(6/7).
[81]
Du Y S;Li X J,Enclaves in the typical mining districts of Tongling,AnHui and their implication to the process of magmatism-metallogeny,Geological Journal of China Universities,1997(02).
[82]
Den J F;Zhao H L;Mo X X,Continental roots-plume tectonics of China:key to continental dynamics,北京:地质出版社,1996.
[83]
Defant M J;Drummond M S,Derivation of some modem magmas by melting of young subduction lithosphere,NATURE,1990.
[84]
Chu G Z;Huang X C;Zhang C H,Diseussion on the orecontrol factors of the Togling area,Anhui,Geology of Anhui,1995(01).
