参考文献/References:
[1] 周涛发,范裕,袁峰.长江中下游成矿带成岩成矿作用研究进展[J].岩石学报, 2008, 24(8): 1665-1678.
[2] 石磊, 楼金伟, 徐晓春. 庐枞盆地中南部铜(金)矿床的流体地球化学特征[J]. 矿床地质, 2010, 29(增刊):601-602.
[3] XIE G Q, MAO J W, ZHU Q Q, et al. Geochemical constraints on Cu-Fe and Fe skarn deposits in the Edong district, Middle-Lower Yangtze River metallogenic belt, China[J]. Ore Geology Reviews, 2015, 64:425-444.
[4] XU G, ZHOU J. The Xinqiao Cu-S-Fe-Au deposit in the Tongling mineral district, China: synorogenic remobilization of a stratiform sulfide deposit[J]. Ore Geology Reviews, 2001, 18(1):77-94.
[5] ZHOU T F, WANG S W, FAN Y, et al. A review of the intracontinental porphyry deposits in the Middle-Lower Yangtze River Valley metallogenic belt, Eastern China[J]. Ore Geology Reviews, 2015, 65(1):433-456.
[6] 翁望飞,王德恩,闫峻, 等.安徽省休宁—歙县地区金多金属矿床 找矿预测地质模型[J].华东地质,2017, 38(3): 184-193.
[7] LIU L M, ZHAO Y L, ZHAO C B. Coupled geodynamics in the formation of Cu skarn deposits in the Tongling-Anqing district, China: Computational modeling and implications for exploration [J]. Journal of Geochemical Exploration, 2010, 106(1/3): 146-155.
[8] 周涛发, 岳书仓, 袁峰. 安徽月山矿田成岩成矿作用[M]. 北京:地质出版社, 2005: 1-265.
[9] 张乐骏, 周涛发, 范裕, 等. 安徽月山岩体的锆石SHRIMP U-Pb定年及其意义[J]. 岩石学报, 2008, 24(8):1725-1732.
[10] 杨光树, 温汉捷, 胡瑞忠, 等. 安徽月山岩体岩石地球化学特征及成因[J]. 矿物学报, 2007, 27(增刊):406-413.
[11] 董树文, 邱瑞龙. 安庆—月山地区构造作用与岩浆活动[M]. 北京:地质出版社, 1993: 1-97.
[12] 刘一男, 范裕, 严四华, 等.长江中下游成矿带安庆-贵池矿集区五横岩体的成岩年代和区域岩浆活动演化研究[J].岩石学报, 2014, 30(4): 1117-1129.
[13] 章贤能,张长松,寇尚文. 安徽宁国东山坞地区金矿地质特征及成因[J]. 华东地质,2019,40(2):114-125.
[14] 欧阳永棚, 尧在雨, 饶建锋, 等. 赣东北景德镇四村矿化蚀变带成矿地质条件及找矿潜力[J]. 华东地质,2019,40(1):51-58.
[15] 张智宇, 杜杨松, 向文帅, 等.安徽安庆铜铁矿床成因:矿床地质特征与元素地球化学约束[J].岩石学报,2012, 28(11): 3739-3756.
[16] LI X, YUAN F, ZHANG M, et al. 3D computational simulation-based mineral prospectivity modeling for exploration for concealed Fe-Cu skarn-type mineralization within the Yueshan orefield, Anqing district, Anhui Province, China [J]. Ore Geology Reviews, 2007,105:1-17.
[17] LIU L, CHU G, LI Y G, et al. Mesozoic High-and Low-SiO2 Adakites and A-Type Granites in the Lower Yangtze River Belt, Eastern China: Implications for Petrogenesis and Metallogeny[J]. Minerals, 2018, 8(8): 1-27.
[18] LIU Z F, SHAO Y J, ZHANG J D, et al. Magma source and evolution law in Yueshan ore field, Anhui Province, China[J]. Journal of Central South University, 2014, 21(4): 1491-1498.
[19] SUN C O, WILLIAMS R J, SUN S S. Distribution coefficients of Eu and Sr for plagioclase-liquid and clinopyroxene-liquid equilibria in oceanic ridge basalt: an experimental study[J]. Geochimica et Cosmochimica Acta, 1974, 38(9): 1415-1433.
[20] SUN S S, MCDONOUGH W F. Chemical and isotopic systematics of oceanic basalts: Implications for mantle composition and processes[J]. Geological Society of London Special Publications, 1989, 42(1): 313-345.
[21] 杨义忠, 王徽, 蔡杨, 等. 北淮阳东段板桥岩体地球化学特征及同位素年代学研究[J]. 华东地质, 2018, 39(4):3-13.
[22] 高守业, 王丽娟, 陆建军, 等. 宁芜和庐枞盆地含矿岩体地球化学特征对比[J]. 华东地质, 2017,38(1): 21-27.
[23] ZHOU T F, FENG Y, YUE S C, et al. Geochemistry and evolution of ore-forming fluids of the Yueshan Cu-Au skarn and vein-type deposits, Anhui Province, South China[J]. Ore Geology Reviews, 2007,31(1/4): 279-303.
[24] 滕传耀,杜杨松,张智宇, 等.安徽安庆铜铁矿床矽卡岩岩相学和矿物学特征及意义[J].矿物岩石, 2012,32(3): 40-50.
[25] 周涛发,袁峰,张鑫, 等.安庆铜牛井热液脉型铜、钼、金矿床石英的40Ar-39Ar快中子活化年龄[J].地质论评, 2003,49(2): 212-216.
[26] 姚国涛. 安徽安庆月山铜铁矿矿田构造研究[D].北京:中国地质大学(北京),2011.
[27] COOPE J A. Geochemical prospecting for porphyry copper-type mineralization: A review[J]. Journal of Geochemical Exploration, 1973,2(2): 81-102.
[28] NEAL L C, WILKINSON J J, MASON P J, et al. Spectral characteristics of propylitic alteration minerals as a vectoring tool for porphyry copper deposits[J]. Journal of Geochemical Exploration, 2018, 184:179-198.
[29] 毛景文,罗茂澄,谢桂青, 等.斑岩铜矿床的基本特征和研究勘查新进展[J].地质学报, 2014,88(12): 2153-2175.
[30] 毛景文,谢桂青,袁顺达, 等.环太平洋成矿带斑岩-矽卡岩型铜矿和与花岗岩有关的锡多金属矿研究现状与展望[J].岩石学报, 2018,34(9): 2501-2517.