安徽安庆月山铜铁矿矿田构造研究
|
摘要
“月山铜铁矿矿田”位于长江中下游铁铜成矿带安庆—贵池矿集区。大地构造位置位于大别山造山带南侧的下扬子台褶带中段,西临淮阳古陆,南靠长江。中生代强烈的挤压收缩环境控制了该区的构造作用,岩浆作用和成矿作用。
本文在前人资料与研究成果的基础之上,结合自己的野外工作,对研究区内的矿田构造形态做了系统详细的整理,结合区域资料建立了研究区的构造演化史,理清区内构造与成矿的关系,希望对研究区内的深部找矿工作有一定的帮助。
形成的主要认识有:
1、理清了矿田内构造与成矿的时间关系。成矿期前主要构造有北东向褶皱,近南北向和近东西向共轭剪裂,以及在成岩过程中热流变导致的围岩褶曲;成矿期是在燕山早期岩体形成之后,期间的主要构造活动是前期构造活动的发展和递变;成矿期后主要是近南北向,北西向及逆冲断层的破矿构造。
2、理清了矿田内构造与成矿的空间关系。矿田内的北东向,近南北向、近东西断裂构造是岩浆上侵的通道,北东向褶皱的倾伏端得层间虚脱则为岩体的赋存提供空间,上述断裂和褶皱构造为导岩和控岩构造。与矿体赋存关系最为密切的是岩体与围岩的接触带构造。矿体赋存位置主要在上述褶曲的层间、核部,围岩凸入岩体的部位,及岩体与围岩接触带的矽卡岩中。
3、查明赋矿层位,即矿田内的矿床在空间上的产出具有一定的“层控”性。矿田范围内的铜铁矿床均分布于月山组含膏碳酸盐岩与月山闪长岩的接触带及其附近。化学性质活泼含膏碳酸盐岩地层,在构造应力的作用下极易破碎和发生层间剥离,形成有利的容岩、容矿空间,化学性质不活泼的铜头尖组粉砂岩,起到了屏蔽效应,抑制了成矿流体的逃逸和散失。
"Yueshan copper-iron ore field" is located in the Anqing -Guichi ore-concentrated area, in the Middle-lower Yangtze River Cu-Fe mineralization belt. Tectonic location is in the middle of lower Yangzi platform fold belt, south of the Dabie orogenic belt, in the near west is huaiyang ancient land, yangtze river is in the south of it. In the environment, strong extrusion and contraction of the Mesozoic Era control the structure effects, magmatic activities and mineralization.
Based on previous material and research results ,with own field work ,this paper make a systemic and detailed consolidation of the ore field structural forms in the research area. In combination with regional materials, established structural evolution in this area, clear the relationship between structures and mineralization. The main comprehensions are as follow:
1. Clear the time relationship between structures and mineralization Before the metallizing period, the main structures are NE face folds, near NS face and near EW face conjugate shear cracks, and the the surrounding rock folds which caused by heat of the diagenetic process. The Metallizing period is behind the formation of magmaticbody in early Yanshanian ,during the period main structures are the former structures’development and progressive deformation. After the metallizing period the structures, including the near NS face and NW face faults and thrust faults, destroy the ore deposits.
2. Clear the spatial relationship between structure and mineralization In the ore field, the fractures of NE face ,near NS face and near EW face are the channels of magma’s invasion. The collapse between the stratums in pitch end of NE face fold provides the space for the. The closest relations with ore’s host is the contact zones between magmaticbody and the surrounding rock .The main locations that hosting ores are in the folds, and skarn in the contact zones.
3. Find out the hosted stratums of ore-deposits, in the ore field deposits have a certain "level control " nature in spatial . The copper iron deposits in the ore field distributes in and near the contact zones between yueshan group gypsum carbonate and the diorite. Carbonate strata of active chemical properties, can easily occur interlayer stripping and crushing under tectonic stress, then form some spaces for ores and magmaticbody. Silty sandstone in tongtoujian group with inactive chemical properties, play a shielding effect and curb the ore-forming fluid’s runaway and lost.
本文在前人资料与研究成果的基础之上,结合自己的野外工作,对研究区内的矿田构造形态做了系统详细的整理,结合区域资料建立了研究区的构造演化史,理清区内构造与成矿的关系,希望对研究区内的深部找矿工作有一定的帮助。
形成的主要认识有:
1、理清了矿田内构造与成矿的时间关系。成矿期前主要构造有北东向褶皱,近南北向和近东西向共轭剪裂,以及在成岩过程中热流变导致的围岩褶曲;成矿期是在燕山早期岩体形成之后,期间的主要构造活动是前期构造活动的发展和递变;成矿期后主要是近南北向,北西向及逆冲断层的破矿构造。
2、理清了矿田内构造与成矿的空间关系。矿田内的北东向,近南北向、近东西断裂构造是岩浆上侵的通道,北东向褶皱的倾伏端得层间虚脱则为岩体的赋存提供空间,上述断裂和褶皱构造为导岩和控岩构造。与矿体赋存关系最为密切的是岩体与围岩的接触带构造。矿体赋存位置主要在上述褶曲的层间、核部,围岩凸入岩体的部位,及岩体与围岩接触带的矽卡岩中。
3、查明赋矿层位,即矿田内的矿床在空间上的产出具有一定的“层控”性。矿田范围内的铜铁矿床均分布于月山组含膏碳酸盐岩与月山闪长岩的接触带及其附近。化学性质活泼含膏碳酸盐岩地层,在构造应力的作用下极易破碎和发生层间剥离,形成有利的容岩、容矿空间,化学性质不活泼的铜头尖组粉砂岩,起到了屏蔽效应,抑制了成矿流体的逃逸和散失。
"Yueshan copper-iron ore field" is located in the Anqing -Guichi ore-concentrated area, in the Middle-lower Yangtze River Cu-Fe mineralization belt. Tectonic location is in the middle of lower Yangzi platform fold belt, south of the Dabie orogenic belt, in the near west is huaiyang ancient land, yangtze river is in the south of it. In the environment, strong extrusion and contraction of the Mesozoic Era control the structure effects, magmatic activities and mineralization.
Based on previous material and research results ,with own field work ,this paper make a systemic and detailed consolidation of the ore field structural forms in the research area. In combination with regional materials, established structural evolution in this area, clear the relationship between structures and mineralization. The main comprehensions are as follow:
1. Clear the time relationship between structures and mineralization Before the metallizing period, the main structures are NE face folds, near NS face and near EW face conjugate shear cracks, and the the surrounding rock folds which caused by heat of the diagenetic process. The Metallizing period is behind the formation of magmaticbody in early Yanshanian ,during the period main structures are the former structures’development and progressive deformation. After the metallizing period the structures, including the near NS face and NW face faults and thrust faults, destroy the ore deposits.
2. Clear the spatial relationship between structure and mineralization In the ore field, the fractures of NE face ,near NS face and near EW face are the channels of magma’s invasion. The collapse between the stratums in pitch end of NE face fold provides the space for the. The closest relations with ore’s host is the contact zones between magmaticbody and the surrounding rock .The main locations that hosting ores are in the folds, and skarn in the contact zones.
3. Find out the hosted stratums of ore-deposits, in the ore field deposits have a certain "level control " nature in spatial . The copper iron deposits in the ore field distributes in and near the contact zones between yueshan group gypsum carbonate and the diorite. Carbonate strata of active chemical properties, can easily occur interlayer stripping and crushing under tectonic stress, then form some spaces for ores and magmaticbody. Silty sandstone in tongtoujian group with inactive chemical properties, play a shielding effect and curb the ore-forming fluid’s runaway and lost.
引文
[1]翟裕生.矿田构造学.北京:地质出版社,1984
[2]翟裕生.关于矿田构造研究的若干问题.地质论评,1984,30(1):19-25
[3]翟裕生.成矿构造研究的回顾和展望.地质论评,2002,48(2):140-146
[4]翟裕生.区域构造、地球化学与成矿.地质调查与研究,2003,26(1):1-7
[5]翟裕生.关于控矿构造研究的思考.矿床地质,13增刊:117-119
[6]翟裕生,姚书振,林新多,等.长江中下游地区铁铜金成矿规律.北京:地质出版社,1992
[7]翟裕生,王建平等.叠加成矿系统与多成因矿床研究.地学前缘,2009,16(6): 282-290
[8]曾庆丰.矿田构造发展特征.地质科学,1982,1:47-56
[9]曾庆丰.矿田构造基础.地质与勘探,1986,22(1):1-6
[10]吴淦国.矿田构造与成矿预测.地质力学学报,1998,4(2):1-4
[11]吴淦国.构造控矿的若干规律.矿床地质,1994,13:62-63
[12]池三川.矿田构造的研究动态.矿床地质,1994,13增刊
[13]翟裕生,邓军,王建平等.深部找矿研究问题.矿床地质,2004,23(4):142-149
[14]邵拥军,彭省临,吴淦国.大型矿山接替资源定位预测的途径及其研究意义.矿产与地质,2005,19(1):16-19
[15]王建平.矿田构造研究方法的技术结构.地质力学学报,1995,1(2):59-65
[16]汪劲草.成矿构造系列的基本问题.桂林工学院学报,2009,29(4):424-433
[17]林新多.南岭及长江中下游矿田构造研究的几个问题.矿床地质,1994:74-76
[18]刘迅.地质力学在矿田构造研究中的应用与进展.地质力学学报,1996,2(1):25-33
[19]常印佛.长江中下游铜铁成矿带.地质出版社, 1991
[20]翟裕生,姚书振,林新多.长江中下游地区铁铜矿床的类型、形成条件和成矿演化.地球科学,1983,22:95-106
[21]邢凤鸣.安徽沿江地区岩浆成矿带.安徽地质,1999,9(4):272-279
[22]蔡本俊.长江中下游地区内生铁铜矿床与膏盐的关系.地球化学,1980,2:193-199
[23]董树文,邱瑞龙.安庆月山地区构造作用与岩浆活动.北京:地质出版社,1993
[24]赵鹏大,李子金,胡光道等.重点成矿区三维立体矿床统计预测—以安徽月山地区为例.武汉:中国地质大学出版社,1992
[25]赵义来,刘亮明,蔡爱良等.安徽安庆铜矿接触带三维形态及其控矿机制分析.地质与勘探,2010,46(4):649-656
[26]李子金.安徽月山地区大比例尺三维立体矿床统计预测的途径和方法.地球科学—中国地质大学学报,1991,16(3):311-317
[27]郭吉保,钱雅倩,黄耀生.安庆矽卡岩矿床的氧同位素交换动力学.火山地质与矿产. 2000, 21(1): 23-29
[28]郭文魁.论安徽铜官山铜矿成因.地质学报, 1957
[29]唐永成,吴言昌,储国正,等.安徽沿江地区铜金多金属矿床地质.北京:地质出版社, 1998
[30]王训诚,周育才.安徽省安庆铜铁矿床地质特征及成因探讨.地质与勘探. 1995, 31(3): 16-24
[31]吴言昌,常印佛.关于岩浆矽卡岩问题.地学前缘,1998,5(4):291-301
[32]邢凤鸣,李志昌.长江中下游早元古代基底的发现及意义.科学通报, 1993, 38(20)
[33]杨光树,温汉捷,胡瑞忠.安庆夕卡岩型铁铜矿床流体包裹体研究.地球化学. 2008, 37(1): 27-36
[34]袁峰,周涛发,刘晓东,等.安徽安庆铜矿床稀土元素地球化学研究.中国稀土学报, 2002, 20(3)
[35]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.岩石学报, 2008, 34(8):1725～1732
[36]陈江峰,李学明,周泰禧等.安徽月山岩体的40Ar/39Ar年龄及与其有关的成矿时代估计.现代地质,1991,5(1):91-99
[37]周涛发,柯韵徽,岳书仓.硅同位素在月山矿田成岩一成矿研究中的应用.合肥工业大学学报(自然科学版). 1996, 19(2): 117-121
[38]周涛发,岳书仓.安徽月山地区闪长岩类地质地球化学研究.火山地质与矿产, 1995, 16(3), 22～3
[39]周涛发,岳书仓.安徽月山地区成岩—成矿作用关系研究.火山地质与矿产,1995,16(2):55-66
[40]周涛发,岳书仓.月山地区铜成矿作用的同位素地球化学研究.矿床地质, 1996, 15(4): 341-350
[41]杜杨松,曹毅,袁万明,等.安徽沿江地区中生代碰撞后到造山后岩浆活动和壳幔相互作用——来自火山-侵入杂岩和岩石包体的证据.岩石学报, 2007, 23(6): 1294-1302
[42]陈星霖.安徽安庆铜矿床地质地球化学特征及成因分析: [硕士学位论文].长沙:中南大学, 2009
[43]李长庆.安徽省安庆铜铁矿床成因及成矿规律研究: [硕士学位论文].长沙:中南工业大学, 2000
[44]于文修.安徽月山岩体成因及其与成矿关系探讨: [硕士学位论文].贵阳:中国科学院贵阳地化所, 2006
[45]向文帅.安徽省安庆大龙山岩体的特征及其地质意义: [学士学位论文].北京:中国地质大学(北京), 2008
[46]赵一鸣,林文蔚,毕承思,等.中国矽卡岩矿床[M].地质出版社,1990
[47]赵一鸣.夕卡岩研究的某些重要新进展.矿床地质, 2002, 21(2), 113～121
[48]中国地质大学(北京).长江中下游地区矽卡岩型矿床成矿规律总结及成矿机制研究项目设计书. 2009
[49]安徽铜都铜业股份有限公司.安徽省铜陵市安庆铜矿接替资源勘查设计书. 2007
[50] Deng JF and Wu ZX.2001.Lithospheric thinning event in the Lower Yangtz Craton and Cu-Fe metallogenic belt in the Middle and Lower Yangtz River reschs.Geology of Anhui,11(2):86～92
[51] Dong Shu-wen,Qiu Rui-long. 1993. Tectonism and magmatism in theAnqing-Yueshan area[M]. 1st Edition. Beijing: Geological Publishing House: 1-18
[52] Chen Jiang- feng, Li Xue-ming, Zhou Tai-x,i K. A. Foland. 1991.40Ar/39Ar Dating for the Yueshan Diorite, Anhui Province and the Estimated FormationTime of the Associated Ore Deposit [J].Geoscience, 5 (1): 91-99
[53] Liu Yu - cheng. 2006. The combination of the integrated prospecting method and the ore-control structure and its application in the Dayeironmine [J].Mineral Deposits, 25 (supp. ): 431-434
[54] Nie Feng-jun, ZhangWan-y,i Du An-dao, Jiang Si-hong, Liu Yan.2007.Re-Os isotopic age dating ofmolybdenite separates from the Chaobuleng skarn iron-polymetallic deposit, Dong Ujimqin Banner, InnerMongolia[ J]. Acta Geoscientica Sinica, 28(4): 315-323
[55] Liu Liang-ming, Shu Zhi-ming, Zhao Chong-bin,Wan Chang-lin,CaiAi- liang, Zhao Yi- lai .2008. The Controlling mechanism of ore Formation due to flow-focusing dilation spaces in Skarn ore deposits and its significance for deep-ore exploration: examples from the Tongling-Anqing district [J].Acta Petrologica Sinica, 24(8):1848 -1856
[56] Mao Jing-wen, LiHong-yan, B Guy, L Raimbault. 1996. Geology and metallogeny of the Shi zhu yuan skarn–greisen W-Sn-Mo-Bide-posit, Hunan province[ J].Mineral Deposits, 15 (1): 1 -15
[57] WangJian-zhong, Li ian-wei ,Zhao Xin-fu, Qian Zhuang-zh,i Ma Chang-qian.2008.Genesis of theChaoshan gold depositand its host intrusion,Tongling area: constraints from 40Ar/39Ar ages and elemental and Sr-Nd-O-C-S isotope geochemistry[J].Acta Petrologica Sinica,24(8):1875-1888
[58] Qiu Rui-long. 1992. Petrological characteristics and genesis of High-K diorites in Yueshan, Anhui province[ J]. Geological Review, 38(2): 98-107
[59] Yan Gui-lin, ZhangMing, LiYong-tao. 1990.On magnetic fabric an palaeomagnetism of the Yueshan pluton, Anqing, Anhui[ J]. Earth Science, 15 (6): 667-673
[60] ZhaoYi-ming,LinWen-we,i Bi Cheng-s,i Li Da-xin. 1986. Basic geological characteristics of skarn deposits of China[ J]. Acta Geosicientia Sinica, 14(3): 59-87
[61] ZhangChuan-ling, Lin Xin-duo, Zhang Shu-zhen. 1994·Ore-controlling regularities of structure in the frontal Zone ofYueshan intrusion in Huaining, Anhui province [ J]. Mineral Deposits, 13(supp. ): 107-109
[62] Li B,Chen JF,Zhao ZF and Qian H.2004.Relationship among oxygen isotope,Rb-Sr isochron and mineral alteration in quartz diorite at yueshan in Anhui.Acta Petrologica Sinica,20(5):1185～1192
[63] Zhou Taofa,Yue Shucang.2000.Basement characteristics and crustal evolution of the copper-gold metallogenic belt in the middle and lower reaches of the Yangtz River: Some isotope constrains.Acta Geologica Sinica,74(2):207～312
[64] Zhou Tao-fa, Liu Xiao-dong, Yuan Feng, Yue Shu-cang. 2001.Migration velocity and scale of the ore-forming fluid for Formation of Cu, Au deposits in Yueshan orefield, Anhui province[J]. GeologicalReview, 47(2): 139-145
[65] Zhou Tao-fa,Yuan Feng,Yue Shu-cang,Liu Xiao-dong, ZhaoYong. 2002.Water/rock interaction during Formation of skarn- type deposits in Yueshan orefield,Anhui province[J].MineralDeposits, 21(1): 1-9
[66] Zhou Tao-fa,Yue Shu-cang. 1997·Formationmechanism of copper deposits in Yueshanorefield, Anhui province[ J]. Journal of ChangchunUniversity of Earth Sciences, 27 (3): 310-316
[67] Zhou Tao-fa,Yue Shu-cang,Yuan Feng. 2005·Lithogenesis of diorites and copper, gold mineralization inYueshan ore field,Anhui province [M]. 1stEdition. Beijing: GeologicalPublishingHouse: 13-17
[68] Zhou TF,Yuan F,Yue S C,LiuX D, ZhangX, FanY. 2007.Geochemistry and evolution of ore- forming fluids of the Yueshan Cu-Au skarn- and vein-yype deposits,Anhuiprovince, SouthChina[J].OreGeologyReviews, 31 (1-4): 279-303
[69] Zhou Taofa,Yue Shucang.1999.Sulfur sources of the copper-gold deposits in the middle and lower reaches of the Yangtz River:An investigation from the Yueshan orefield .Scientia Geologica Sininca,8(1):31～40
[2]翟裕生.关于矿田构造研究的若干问题.地质论评,1984,30(1):19-25
[3]翟裕生.成矿构造研究的回顾和展望.地质论评,2002,48(2):140-146
[4]翟裕生.区域构造、地球化学与成矿.地质调查与研究,2003,26(1):1-7
[5]翟裕生.关于控矿构造研究的思考.矿床地质,13增刊:117-119
[6]翟裕生,姚书振,林新多,等.长江中下游地区铁铜金成矿规律.北京:地质出版社,1992
[7]翟裕生,王建平等.叠加成矿系统与多成因矿床研究.地学前缘,2009,16(6): 282-290
[8]曾庆丰.矿田构造发展特征.地质科学,1982,1:47-56
[9]曾庆丰.矿田构造基础.地质与勘探,1986,22(1):1-6
[10]吴淦国.矿田构造与成矿预测.地质力学学报,1998,4(2):1-4
[11]吴淦国.构造控矿的若干规律.矿床地质,1994,13:62-63
[12]池三川.矿田构造的研究动态.矿床地质,1994,13增刊
[13]翟裕生,邓军,王建平等.深部找矿研究问题.矿床地质,2004,23(4):142-149
[14]邵拥军,彭省临,吴淦国.大型矿山接替资源定位预测的途径及其研究意义.矿产与地质,2005,19(1):16-19
[15]王建平.矿田构造研究方法的技术结构.地质力学学报,1995,1(2):59-65
[16]汪劲草.成矿构造系列的基本问题.桂林工学院学报,2009,29(4):424-433
[17]林新多.南岭及长江中下游矿田构造研究的几个问题.矿床地质,1994:74-76
[18]刘迅.地质力学在矿田构造研究中的应用与进展.地质力学学报,1996,2(1):25-33
[19]常印佛.长江中下游铜铁成矿带.地质出版社, 1991
[20]翟裕生,姚书振,林新多.长江中下游地区铁铜矿床的类型、形成条件和成矿演化.地球科学,1983,22:95-106
[21]邢凤鸣.安徽沿江地区岩浆成矿带.安徽地质,1999,9(4):272-279
[22]蔡本俊.长江中下游地区内生铁铜矿床与膏盐的关系.地球化学,1980,2:193-199
[23]董树文,邱瑞龙.安庆月山地区构造作用与岩浆活动.北京:地质出版社,1993
[24]赵鹏大,李子金,胡光道等.重点成矿区三维立体矿床统计预测—以安徽月山地区为例.武汉:中国地质大学出版社,1992
[25]赵义来,刘亮明,蔡爱良等.安徽安庆铜矿接触带三维形态及其控矿机制分析.地质与勘探,2010,46(4):649-656
[26]李子金.安徽月山地区大比例尺三维立体矿床统计预测的途径和方法.地球科学—中国地质大学学报,1991,16(3):311-317
[27]郭吉保,钱雅倩,黄耀生.安庆矽卡岩矿床的氧同位素交换动力学.火山地质与矿产. 2000, 21(1): 23-29
[28]郭文魁.论安徽铜官山铜矿成因.地质学报, 1957
[29]唐永成,吴言昌,储国正,等.安徽沿江地区铜金多金属矿床地质.北京:地质出版社, 1998
[30]王训诚,周育才.安徽省安庆铜铁矿床地质特征及成因探讨.地质与勘探. 1995, 31(3): 16-24
[31]吴言昌,常印佛.关于岩浆矽卡岩问题.地学前缘,1998,5(4):291-301
[32]邢凤鸣,李志昌.长江中下游早元古代基底的发现及意义.科学通报, 1993, 38(20)
[33]杨光树,温汉捷,胡瑞忠.安庆夕卡岩型铁铜矿床流体包裹体研究.地球化学. 2008, 37(1): 27-36
[34]袁峰,周涛发,刘晓东,等.安徽安庆铜矿床稀土元素地球化学研究.中国稀土学报, 2002, 20(3)
[35]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.岩石学报, 2008, 34(8):1725～1732
[36]陈江峰,李学明,周泰禧等.安徽月山岩体的40Ar/39Ar年龄及与其有关的成矿时代估计.现代地质,1991,5(1):91-99
[37]周涛发,柯韵徽,岳书仓.硅同位素在月山矿田成岩一成矿研究中的应用.合肥工业大学学报(自然科学版). 1996, 19(2): 117-121
[38]周涛发,岳书仓.安徽月山地区闪长岩类地质地球化学研究.火山地质与矿产, 1995, 16(3), 22～3
[39]周涛发,岳书仓.安徽月山地区成岩—成矿作用关系研究.火山地质与矿产,1995,16(2):55-66
[40]周涛发,岳书仓.月山地区铜成矿作用的同位素地球化学研究.矿床地质, 1996, 15(4): 341-350
[41]杜杨松,曹毅,袁万明,等.安徽沿江地区中生代碰撞后到造山后岩浆活动和壳幔相互作用——来自火山-侵入杂岩和岩石包体的证据.岩石学报, 2007, 23(6): 1294-1302
[42]陈星霖.安徽安庆铜矿床地质地球化学特征及成因分析: [硕士学位论文].长沙:中南大学, 2009
[43]李长庆.安徽省安庆铜铁矿床成因及成矿规律研究: [硕士学位论文].长沙:中南工业大学, 2000
[44]于文修.安徽月山岩体成因及其与成矿关系探讨: [硕士学位论文].贵阳:中国科学院贵阳地化所, 2006
[45]向文帅.安徽省安庆大龙山岩体的特征及其地质意义: [学士学位论文].北京:中国地质大学(北京), 2008
[46]赵一鸣,林文蔚,毕承思,等.中国矽卡岩矿床[M].地质出版社,1990
[47]赵一鸣.夕卡岩研究的某些重要新进展.矿床地质, 2002, 21(2), 113～121
[48]中国地质大学(北京).长江中下游地区矽卡岩型矿床成矿规律总结及成矿机制研究项目设计书. 2009
[49]安徽铜都铜业股份有限公司.安徽省铜陵市安庆铜矿接替资源勘查设计书. 2007
[50] Deng JF and Wu ZX.2001.Lithospheric thinning event in the Lower Yangtz Craton and Cu-Fe metallogenic belt in the Middle and Lower Yangtz River reschs.Geology of Anhui,11(2):86～92
[51] Dong Shu-wen,Qiu Rui-long. 1993. Tectonism and magmatism in theAnqing-Yueshan area[M]. 1st Edition. Beijing: Geological Publishing House: 1-18
[52] Chen Jiang- feng, Li Xue-ming, Zhou Tai-x,i K. A. Foland. 1991.40Ar/39Ar Dating for the Yueshan Diorite, Anhui Province and the Estimated FormationTime of the Associated Ore Deposit [J].Geoscience, 5 (1): 91-99
[53] Liu Yu - cheng. 2006. The combination of the integrated prospecting method and the ore-control structure and its application in the Dayeironmine [J].Mineral Deposits, 25 (supp. ): 431-434
[54] Nie Feng-jun, ZhangWan-y,i Du An-dao, Jiang Si-hong, Liu Yan.2007.Re-Os isotopic age dating ofmolybdenite separates from the Chaobuleng skarn iron-polymetallic deposit, Dong Ujimqin Banner, InnerMongolia[ J]. Acta Geoscientica Sinica, 28(4): 315-323
[55] Liu Liang-ming, Shu Zhi-ming, Zhao Chong-bin,Wan Chang-lin,CaiAi- liang, Zhao Yi- lai .2008. The Controlling mechanism of ore Formation due to flow-focusing dilation spaces in Skarn ore deposits and its significance for deep-ore exploration: examples from the Tongling-Anqing district [J].Acta Petrologica Sinica, 24(8):1848 -1856
[56] Mao Jing-wen, LiHong-yan, B Guy, L Raimbault. 1996. Geology and metallogeny of the Shi zhu yuan skarn–greisen W-Sn-Mo-Bide-posit, Hunan province[ J].Mineral Deposits, 15 (1): 1 -15
[57] WangJian-zhong, Li ian-wei ,Zhao Xin-fu, Qian Zhuang-zh,i Ma Chang-qian.2008.Genesis of theChaoshan gold depositand its host intrusion,Tongling area: constraints from 40Ar/39Ar ages and elemental and Sr-Nd-O-C-S isotope geochemistry[J].Acta Petrologica Sinica,24(8):1875-1888
[58] Qiu Rui-long. 1992. Petrological characteristics and genesis of High-K diorites in Yueshan, Anhui province[ J]. Geological Review, 38(2): 98-107
[59] Yan Gui-lin, ZhangMing, LiYong-tao. 1990.On magnetic fabric an palaeomagnetism of the Yueshan pluton, Anqing, Anhui[ J]. Earth Science, 15 (6): 667-673
[60] ZhaoYi-ming,LinWen-we,i Bi Cheng-s,i Li Da-xin. 1986. Basic geological characteristics of skarn deposits of China[ J]. Acta Geosicientia Sinica, 14(3): 59-87
[61] ZhangChuan-ling, Lin Xin-duo, Zhang Shu-zhen. 1994·Ore-controlling regularities of structure in the frontal Zone ofYueshan intrusion in Huaining, Anhui province [ J]. Mineral Deposits, 13(supp. ): 107-109
[62] Li B,Chen JF,Zhao ZF and Qian H.2004.Relationship among oxygen isotope,Rb-Sr isochron and mineral alteration in quartz diorite at yueshan in Anhui.Acta Petrologica Sinica,20(5):1185～1192
[63] Zhou Taofa,Yue Shucang.2000.Basement characteristics and crustal evolution of the copper-gold metallogenic belt in the middle and lower reaches of the Yangtz River: Some isotope constrains.Acta Geologica Sinica,74(2):207～312
[64] Zhou Tao-fa, Liu Xiao-dong, Yuan Feng, Yue Shu-cang. 2001.Migration velocity and scale of the ore-forming fluid for Formation of Cu, Au deposits in Yueshan orefield, Anhui province[J]. GeologicalReview, 47(2): 139-145
[65] Zhou Tao-fa,Yuan Feng,Yue Shu-cang,Liu Xiao-dong, ZhaoYong. 2002.Water/rock interaction during Formation of skarn- type deposits in Yueshan orefield,Anhui province[J].MineralDeposits, 21(1): 1-9
[66] Zhou Tao-fa,Yue Shu-cang. 1997·Formationmechanism of copper deposits in Yueshanorefield, Anhui province[ J]. Journal of ChangchunUniversity of Earth Sciences, 27 (3): 310-316
[67] Zhou Tao-fa,Yue Shu-cang,Yuan Feng. 2005·Lithogenesis of diorites and copper, gold mineralization inYueshan ore field,Anhui province [M]. 1stEdition. Beijing: GeologicalPublishingHouse: 13-17
[68] Zhou TF,Yuan F,Yue S C,LiuX D, ZhangX, FanY. 2007.Geochemistry and evolution of ore- forming fluids of the Yueshan Cu-Au skarn- and vein-yype deposits,Anhuiprovince, SouthChina[J].OreGeologyReviews, 31 (1-4): 279-303
[69] Zhou Taofa,Yue Shucang.1999.Sulfur sources of the copper-gold deposits in the middle and lower reaches of the Yangtz River:An investigation from the Yueshan orefield .Scientia Geologica Sininca,8(1):31～40