［1］Chang Y F, Liu X P and Wu Y C. 1991. The Cu, Fe metallogenic belt in the middle-lower reaches of Yangtze River.[M]. Beijing: Geol. Pub. House. 1～379(in Chinese).
[2]
［2］Deng J, Huang D H, Wang Q F, et al. 2004. The formation mechanism of the "Drag Depressions" and the irregular boundaries in intraplate deformation [J]. Acta Geologica Sinica, 78(1):267～272.
[3]
［3］Deng J F, Dai S Q, Zhao H L, et al. 2002. Recognition of magenic systems and subsystems in Tongling Cu-Au(Ag) ore-formingarea[J]. Mineral Deposits, 21(4): 317～322(in Chinese with English abstract).
[4]
［4］Huang D H and Zhong G H. 1994. Experimental study and dynamic analysis of Indosinian-Yanshanian regional tectomc deformation in Southeart Hubei[J]. Mineral deposits, 13(4): 209～307(in Chinese with English abstract).
[5]
［5］Pan Y M and Dong P. 1999. The Lower Changjiang (Yangzi/Yangtze River) metallogenic belt, east central China: intrusion- and wall rock-hosted Cu-Fe-Au, Mo, Zn, Pb, Ag deposits[J].Ore Geology Reviews, 15 (4): 177～242.
[6]
［6］Wu C L, Wang F S, Hao M Y, et al. 2000a. Geochronology of Intermediate-Acid Intrusive Rocks from Tongling, Anhui[J]. Continental Dynamics, 5(1):15～23.
[7]
［7］Xu G and Lin X. 2000. Geology and geochemistry of the Changlongshan skarn iron deposit, Anhui Province, China [J].Ore Geology Reviews,16 (1～2): 91～106.
[8]
［8］Xu G and Zhou J. 2001.The Xinqiao Cu-S-Fe-Au deposit in the Tongling mineral district, China: synorogenic remobilization of a stratiform sulfide deposit [J]. Ore Geology Reviews, 18 (1～2): 77～94.
[9]
［9］Zhai Y S, Yao S Z and Lin X D. 1992.The metallogenic law of Fe and Cu (Au) in the middle and lower reaches of the Changjiang River[M]. Beijing: Geol. Pub. House. 1～235(in Chinese).
