铜陵新桥Cu-S-Fe矿床下盘石英黄铁矿脉石英流体包裹体Rb-Sr同位素定年
|
摘要
为了探讨新桥Cu—S—Fe矿床的形成是否经历过海西期海底喷流沉积成矿作用,在详细的野外调研和室内工作基础上,对层状矿体下盘石英黄铁矿脉中的石英流体包裹体进行Rb-Sr同位素定年分析。研究结果表明:下盘石英黄铁矿脉中的石英流体包裹体Rb-Sr等时线年龄为138.0±2.3Ma(MSWD=5.4),与矶头复式岩株的成岩年龄相近(140.4±2.2Ma),而且下盘网脉状矿化石英流体包裹体中流体的n(~(87)Sr)/n(~(86)Sr)初始值(0.71138±0.00014)和矶头岩株的n(~(87)Sr)/n(~(86)Sr)初始比值相近,说明下盘网脉状矿化为岩浆热液成因,并非为海西期海底喷流通道。与典型海底喷流沉积矿床进行地质特征对比分析也发现,新桥Cu—S—Fe矿床地质特征有别于典型的海底喷流沉积矿床。综合分析认为,新桥Cu—S—Fe矿床应属于燕山期岩浆热液矿床。
In order to investigate whether Xinqiao Cu—S—Fe deposit experienced Hercynian Sedex mineralization,Rb-Sr isotope analysis of fluid inclusion in quartz from stockwork mineralization of footwall in Xinqiao Cu—S—Fe deposit,based on detailed field investigation and laboratory work.The results indicate that the Rb-Sr isochron age of fluid inclusion in quartz from stockwork mineralization of footwall is 138.0 ±2.3Ma(MSWD= 5.4),close to the weighted average age of zircons in Jitou Rock Strain(140.4 ± 2.2Ma),and the Sr/ Sr initial value is 0.71138 ±0.00014,close to the one of Jitou Rock Strain.Form the dating data,we get that stockwork mineralization of footwall formed for magmatic hydrothermal,not for the Sedex mineralization in Hercynian.The comparison between typical Sedex type deposit and Xinqiao Cu—S—Fe deposit suggests that the geological characteristics of Xinqiao Cu—S—Fe deposit is different form typical Sedex deposit,obviously.Comprehensive analysis shows that Xinqiao Cu—S—Fe deposit didn 't experience Sedex mineralization in Hercynian.
In order to investigate whether Xinqiao Cu—S—Fe deposit experienced Hercynian Sedex mineralization,Rb-Sr isotope analysis of fluid inclusion in quartz from stockwork mineralization of footwall in Xinqiao Cu—S—Fe deposit,based on detailed field investigation and laboratory work.The results indicate that the Rb-Sr isochron age of fluid inclusion in quartz from stockwork mineralization of footwall is 138.0 ±2.3Ma(MSWD= 5.4),close to the weighted average age of zircons in Jitou Rock Strain(140.4 ± 2.2Ma),and the Sr/ Sr initial value is 0.71138 ±0.00014,close to the one of Jitou Rock Strain.Form the dating data,we get that stockwork mineralization of footwall formed for magmatic hydrothermal,not for the Sedex mineralization in Hercynian.The comparison between typical Sedex type deposit and Xinqiao Cu—S—Fe deposit suggests that the geological characteristics of Xinqiao Cu—S—Fe deposit is different form typical Sedex deposit,obviously.Comprehensive analysis shows that Xinqiao Cu—S—Fe deposit didn 't experience Sedex mineralization in Hercynian.
引文
常印佛,刘湘培,吴言昌.1991.长江中下游铜铁成矿带.北京:地质出版社,1~379.
常印佛,刘学圭.1983.层控式矽卡岩型矿床——以安徽省内下扬子坳陷中一些矿床为例.矿床地质,2(1):11~20.
陈彬.2003.新桥硫~多金属矿床含硫磁铁矿体地质特征及成因探讨.化工矿产地质,25(3):173~178.
陈好寿,李华芹.1991.云开隆起金矿带流体包裹体Rb-Sr等时线年龄.矿床地质,10(04):333~341.
顾连兴,徐克勤.1986.论长江中下游中石炭世海底块状硫化钨矿床.地质学报,60(2):176~188.
郭维民,陆建军,蒋少涌,章荣清,漆亮.2011.安徽铜陵新桥矿床下盘矿化中黄铁矿Re-Os同位素定年:海底喷流沉积成矿的年代学证据.科学通报,56(36):3023~3028.
郭春丽,王登红,陈毓川,王彦斌,陈郑辉,刘善宝.2007.赣南中生代淘锡坑钨矿区花岗岩锆石SHRIMP年龄及石英脉Rb-Sr年龄测定.矿床地质,26(4):432~442.
李红阳,李英杰,侯增谦,杨竹森,蒙义峰,曾普胜,徐文艺.2005.安徽新桥块状硫化物矿床地球化学特征.地质科学,40(3):337~345.
李红阳,李英杰,康桂玲,曹积飞,杨竹森,侯增谦,蒙义峰.2008.安徽铜官山铜—铁-金-硫矿床的地球化学特征.地质科学,43(2):370~376.
李华芹,刘家齐,杜国民,魏林.1992.内生金属矿床成矿作用年代学研究:以西华山钨矿为例.科学通报,37(12):1109~1112.
李文达,王文斌,范洪源.1997.长江中下游铜(金)矿床密集区形成条件和超大型矿床存在的可能性.火山地质与矿产,20(S):1~131.
刘建明,赵善仁,沈洁,姜能,霍卫国.1998.地质流体活动的同位素定年方法评述.地球物理学报,13(3):46~55.
刘文灿,高德臻,储国正.1996.安徽铜陵地区构造变形分析及成矿预测.北京:地质出版社,1~131.
刘心兵.2002.新桥硫铁矿矿床地质特征及控矿因素分析.矿业快报,(22),13~15.
刘裕庆.1991.铜陵地区层状铜(铁硫)矿床同位素地球化学研究.北京:地质出版社,47~82.
毛光周,华仁民,龙光明,陆慧娟.2008.江西金山金矿成矿时代探讨——来自石英流体包裹体Ro-Sr年龄的证据.地质学报,82(4)532~539.
毛景文,邵拥军,谢桂青,张建东,陈毓川.2009.长江中下游成矿带铜陵矿集区铜多金属矿床模型,矿床地质,28(2):109~119.
毛景文,张作衡,余金杰,王义天,牛宝贵.2003.华北及邻区中生代大规模成矿的地球动力学背景:从金属矿床精确年龄得到的启示.中国科学(D辑),33(4):289~299.
莫测辉,王秀璋,程景平,梁华英.1997.冀西北东坪金矿床含金石英脉石英流体包裹体Rb-Sr等时线及其地质意义.地球化学,26(3):20~27.
戚建中,刘红樱,姜耀辉.2000.中国东部燕山期俯冲走滑体制及其对成矿定位的控制.火山地质与矿产,21(4):244~266.
孙敬博,张立明,陈文,李华芹,张彦,刘新宇,李洁,张斌.2013.东天山红石金矿床石英Rb-Sr同位素定年.地质论评,59(2):382~388.
唐永成,吴言昌,储国正,邢凤鸣,王永敏,曹奋扬,常印佛.1998.安徽沿江地区铜金多金属矿床地质.北京:地质出版社,1~351.
王恩德,王荣湖.1991.铜陵新桥铁帽金矿床中金赋存特征及富集规律.沈阳黄金学院学报,10(3):1~10.
王国光,倪培.2009.新桥多金属矿床的矿体下部网脉状矿化的流体包裹体研究.矿物学报,29(S1):256.
王秀璋,单强,梁华英,程景平,夏萍.1999.金山金矿床成矿时代及矿床成因.地球化学,28(1):10~17.
王彦斌,唐索寒,王进辉,曾普胜,杨竹森,蒙义峰,田世洪.2004.安徽铜陵新桥铜金矿床黄铁矿Rb/Sr同位素年龄数据——燕山晚期成矿作用的证据.地质论评,50(5):538~541.
王玉奇.2009.Sedex型矿床与VMS型矿床对比研究.资源环境与工程,23(3):259~262.
王跃,朱祥坤.2009.安徽新桥硫铁矿矿床的Fe同位素初步研究.矿物学报,29(S1):615~616.
王跃,朱祥坤,程彦博,李志红.2013.安徽新桥矿床矿相学与Fe同位素特征及其对矿床成因的制约.吉林大学学报(地球科学版),43(6):1787~1798.
吴福元,葛文春,孙德有,郭春丽.2003.中国东部岩石圈减薄研究中的几个问题.地学前缘,10(3):51~60.
肖新建,倪培,2000,论喷流沉积(SEDEX)成矿与沉积-改造成矿之对比,地质找矿论丛,15(3):238~245.
谢华光,王文斌,李文达.1995.安徽新桥铜硫矿床成矿时代及成矿物质来源.火山地质与矿产,16(2):101~107.
谢建成,杨晓勇,杜建国,杜小伟,肖益林,屈文俊,孙卫东.2009.安徽铜陵新桥Cu—Au—Fe—S矿床黄铁矿Re-Os定年及成矿意义.地质科学,44(1):183~192.
徐克勤,朱金初.1978.我国东南部几个断裂坳陷带中沉积(或火山沉积)热液叠加类型铜矿床成因的探讨.福建地质,4:1~68.
徐文艺,杨竹森,蒙义峰,曾普胜,史大年,田世洪,李红阳.2004.安徽铜陵矿集区块状硫化物矿床成因模型与成矿流体动力学迁.矿床地质,23(3):353~364.
徐应龙,郭继伟.2009.安徽省铜陵县新桥铁帽金银矿床地球化学特征.现代矿业,(8):92~95.
薛良伟,庞继群,王祥国,周长命.1999.小秦岭303号石英脉流体包裹体Rb-Sr、~(40)Ar-~(39)Ar成矿年龄测定.地球化学,28(5):473~478.
阎学义,袁成详.1977.长江中下游成矿带中石炭世海底火山喷发-沉积黄铁矿型铜矿地质特征.南京大学学报(自然科学版),(1):43~67.
杨兵,王之田.1985.铜官山铜矿床新类型矿体的发现及矿床成因模式——兼论其与区域铜矿复合模式的关系.矿床地质,4(4):1~13.
杨道斐,傅德鑫,吴履秀.1982.从矿石成分及结构构造特征看新桥及其邻近地区黄铁矿型铜矿床的成因.中国地质科学院南京地质矿产研究所所刊,3(4):59~68.
姚海涛,郑海飞.2001.流体包裹体Rb-Sr等时线定年的可靠性.地球化学,30(6):507~511.
於崇文,岑况,鲍征宇.1998.成矿作用动力学.北京:地质出版社:1~224.
岳文浙,魏乃甄,焦世鼎.1993.长江中下游威宁期沉积地质与块状硫化物矿床.北京:地质出版社,50~78.
臧文拴,吴淦国,张达,刘爱华.2004.铜陵新桥铁矿田地质地球化学特征及成因浅析.大地构造与成矿学,28(2):187~193.
翟伟,李兆麟,黄栋林,文拥军.2004.粤西河台金矿床富硫化物石英脉Rb-Sr等时线年龄讨论.地球学报,25(2):2443~247.
翟裕生,姚书振,林新多,金福全,周珣若,万天丰,周宗桂.1992.长江中下游地区铁、铜等成矿规律研究.矿床地质,11(1):1~235.
张德贵.1982.安徽最大铜硫矿床地质概要——论新桥铜硫铁矿床的成因.地质科技情报,(S1):73~75.
张宇.201 1.安徽铜陵新桥铜硫铁矿床地质地球化学特征及矿床成因分析.导师:邵拥军.长沙:中南大学地球科学与信息物理学院硕士学位论文:1~98.
张宇,邵拥军,周鑫,刘忠法,郑明泓.2013.安徽铜陵新桥铜硫铁矿床胶状黄铁矿主、微量元素特征.中国有色金属学报,23(12):3492~3502.
郑培玺,周燕,王铁夫,张延洁.2007.山东招远灵雀山金矿床富金石英脉铷-锶等时线年龄讨论.岩矿测试,26(5):356~358.
周强强,胡文洁.2012.Sr同位素的研究现状和最新进展.科技信息,1:396.
周涛发,范裕,袁峰.2008.长江中下游成矿带成岩成矿作用研究进展.岩石学报,24(8):1665~1678.
周涛发,岳书仓.2000.长假中下游两个系列铜金矿床成矿流体系统的形成条件及机理.北京大学学报(自然科学版),36(5):697~707.
周涛发,张乐骏,袁峰,范裕,David R.Cooke.2010.安徽铜陵新桥Cu—Au—S矿床黄铁矿微量元素LA-ICP-MS原位测定及其对矿床成因的制约.地学前缘,17(2):306~319.
Cu Lianxing,Hu Wenxuan,He Jinxiang,Ni Pei,Xu Keqin.2000.Regional variations in ore composition and fluid features of massive sulfide deposits in South China:Implications for genetic modeling.Episodes,23(2):110~118.
John F S,Julie A D,Jeanine M S,Lorn E E Y,Cameron S R.Paleozoic sedimentary rocks in the Red Dog Zn—Pb—Ag district and Vicinity,Western Brooks Range,Alaska:Provenance,deposition and metallogenic significance for the genesis of the orebodies.Economic Geology,2004,99(7):1385~1414.
Ludwing K R.2001.ISOPLOT/Ex.Version 2.49.A Geochronological Toolkit for Microsoft Excel.Berkeley Geochronology Center,1~20.
Mao Jingwen,Xie Guiqing,Duan Chao,Franco Pirajno,Dazio Ishiyama,Chen Yuchuan.2011.A Tectono-Genetic Model for Porphyry-Skarn-Stratabound Cu—Au—Fe and Magnetite—Apatite Deposit Along the Middle—Lower Yangtze River Valley,Eastern China.Ore Geology Reviews,2011,43(1):294~314.
Pan Yuanming,Done Ping.1999.The lower Changjiang(Yangtzi/Yangtze River)metallogenic belt,east—center China:intrusion and wall rock hosted Cu—Fe—Au,Mo,Zn,Pb,Ag deposits.Ore Geology Reviews,15(4):177~242.
Pettke T,Diamond L W.1995.Rb-Sr isotopic analysis of fluid inclusions in quartz.-Evaluation of bulk extraction procedure and geochronometer systematics using synthetic fluid inclusions.Geochimica et Cosmochimica Acta,59:4009~4027.
Rossman G R,Weis D,Wasserburg G J.1987.Rb,Sr,Nd and Sm concentrations in quartz.Geochmiica et Cosmochmiica Acta,51:2325~2329.
Shepherd T J,Darbyshire D P E.1982.Fluid inclusion Rb-Sr isochrones for dating mineral deposits.Narture,1981,290:578~579.
Wang Yue,Zhu X iangkun,Mao Jingwen,Li Zhihonh,Cheng Yanbo.2011.Iron Isotope Fractionation During Skarn-Type Metallogeny:A Case Study of Xiao Cu—S—Fe—Au Deposit in the Middle—Lower Yangtze Valley.Ore Geology Reviews,43:194~202.
Xu G,Zhou J.2001.The Xinqiao Cu—S—Fe—Au deposit in the Tongling mineral district,China:synorogenic remobilization of a stratiform sulfide deposit.Ore Geology Reviews,18:77~94.
常印佛,刘学圭.1983.层控式矽卡岩型矿床——以安徽省内下扬子坳陷中一些矿床为例.矿床地质,2(1):11~20.
陈彬.2003.新桥硫~多金属矿床含硫磁铁矿体地质特征及成因探讨.化工矿产地质,25(3):173~178.
陈好寿,李华芹.1991.云开隆起金矿带流体包裹体Rb-Sr等时线年龄.矿床地质,10(04):333~341.
顾连兴,徐克勤.1986.论长江中下游中石炭世海底块状硫化钨矿床.地质学报,60(2):176~188.
郭维民,陆建军,蒋少涌,章荣清,漆亮.2011.安徽铜陵新桥矿床下盘矿化中黄铁矿Re-Os同位素定年:海底喷流沉积成矿的年代学证据.科学通报,56(36):3023~3028.
郭春丽,王登红,陈毓川,王彦斌,陈郑辉,刘善宝.2007.赣南中生代淘锡坑钨矿区花岗岩锆石SHRIMP年龄及石英脉Rb-Sr年龄测定.矿床地质,26(4):432~442.
李红阳,李英杰,侯增谦,杨竹森,蒙义峰,曾普胜,徐文艺.2005.安徽新桥块状硫化物矿床地球化学特征.地质科学,40(3):337~345.
李红阳,李英杰,康桂玲,曹积飞,杨竹森,侯增谦,蒙义峰.2008.安徽铜官山铜—铁-金-硫矿床的地球化学特征.地质科学,43(2):370~376.
李华芹,刘家齐,杜国民,魏林.1992.内生金属矿床成矿作用年代学研究:以西华山钨矿为例.科学通报,37(12):1109~1112.
李文达,王文斌,范洪源.1997.长江中下游铜(金)矿床密集区形成条件和超大型矿床存在的可能性.火山地质与矿产,20(S):1~131.
刘建明,赵善仁,沈洁,姜能,霍卫国.1998.地质流体活动的同位素定年方法评述.地球物理学报,13(3):46~55.
刘文灿,高德臻,储国正.1996.安徽铜陵地区构造变形分析及成矿预测.北京:地质出版社,1~131.
刘心兵.2002.新桥硫铁矿矿床地质特征及控矿因素分析.矿业快报,(22),13~15.
刘裕庆.1991.铜陵地区层状铜(铁硫)矿床同位素地球化学研究.北京:地质出版社,47~82.
毛光周,华仁民,龙光明,陆慧娟.2008.江西金山金矿成矿时代探讨——来自石英流体包裹体Ro-Sr年龄的证据.地质学报,82(4)532~539.
毛景文,邵拥军,谢桂青,张建东,陈毓川.2009.长江中下游成矿带铜陵矿集区铜多金属矿床模型,矿床地质,28(2):109~119.
毛景文,张作衡,余金杰,王义天,牛宝贵.2003.华北及邻区中生代大规模成矿的地球动力学背景:从金属矿床精确年龄得到的启示.中国科学(D辑),33(4):289~299.
莫测辉,王秀璋,程景平,梁华英.1997.冀西北东坪金矿床含金石英脉石英流体包裹体Rb-Sr等时线及其地质意义.地球化学,26(3):20~27.
戚建中,刘红樱,姜耀辉.2000.中国东部燕山期俯冲走滑体制及其对成矿定位的控制.火山地质与矿产,21(4):244~266.
孙敬博,张立明,陈文,李华芹,张彦,刘新宇,李洁,张斌.2013.东天山红石金矿床石英Rb-Sr同位素定年.地质论评,59(2):382~388.
唐永成,吴言昌,储国正,邢凤鸣,王永敏,曹奋扬,常印佛.1998.安徽沿江地区铜金多金属矿床地质.北京:地质出版社,1~351.
王恩德,王荣湖.1991.铜陵新桥铁帽金矿床中金赋存特征及富集规律.沈阳黄金学院学报,10(3):1~10.
王国光,倪培.2009.新桥多金属矿床的矿体下部网脉状矿化的流体包裹体研究.矿物学报,29(S1):256.
王秀璋,单强,梁华英,程景平,夏萍.1999.金山金矿床成矿时代及矿床成因.地球化学,28(1):10~17.
王彦斌,唐索寒,王进辉,曾普胜,杨竹森,蒙义峰,田世洪.2004.安徽铜陵新桥铜金矿床黄铁矿Rb/Sr同位素年龄数据——燕山晚期成矿作用的证据.地质论评,50(5):538~541.
王玉奇.2009.Sedex型矿床与VMS型矿床对比研究.资源环境与工程,23(3):259~262.
王跃,朱祥坤.2009.安徽新桥硫铁矿矿床的Fe同位素初步研究.矿物学报,29(S1):615~616.
王跃,朱祥坤,程彦博,李志红.2013.安徽新桥矿床矿相学与Fe同位素特征及其对矿床成因的制约.吉林大学学报(地球科学版),43(6):1787~1798.
吴福元,葛文春,孙德有,郭春丽.2003.中国东部岩石圈减薄研究中的几个问题.地学前缘,10(3):51~60.
肖新建,倪培,2000,论喷流沉积(SEDEX)成矿与沉积-改造成矿之对比,地质找矿论丛,15(3):238~245.
谢华光,王文斌,李文达.1995.安徽新桥铜硫矿床成矿时代及成矿物质来源.火山地质与矿产,16(2):101~107.
谢建成,杨晓勇,杜建国,杜小伟,肖益林,屈文俊,孙卫东.2009.安徽铜陵新桥Cu—Au—Fe—S矿床黄铁矿Re-Os定年及成矿意义.地质科学,44(1):183~192.
徐克勤,朱金初.1978.我国东南部几个断裂坳陷带中沉积(或火山沉积)热液叠加类型铜矿床成因的探讨.福建地质,4:1~68.
徐文艺,杨竹森,蒙义峰,曾普胜,史大年,田世洪,李红阳.2004.安徽铜陵矿集区块状硫化物矿床成因模型与成矿流体动力学迁.矿床地质,23(3):353~364.
徐应龙,郭继伟.2009.安徽省铜陵县新桥铁帽金银矿床地球化学特征.现代矿业,(8):92~95.
薛良伟,庞继群,王祥国,周长命.1999.小秦岭303号石英脉流体包裹体Rb-Sr、~(40)Ar-~(39)Ar成矿年龄测定.地球化学,28(5):473~478.
阎学义,袁成详.1977.长江中下游成矿带中石炭世海底火山喷发-沉积黄铁矿型铜矿地质特征.南京大学学报(自然科学版),(1):43~67.
杨兵,王之田.1985.铜官山铜矿床新类型矿体的发现及矿床成因模式——兼论其与区域铜矿复合模式的关系.矿床地质,4(4):1~13.
杨道斐,傅德鑫,吴履秀.1982.从矿石成分及结构构造特征看新桥及其邻近地区黄铁矿型铜矿床的成因.中国地质科学院南京地质矿产研究所所刊,3(4):59~68.
姚海涛,郑海飞.2001.流体包裹体Rb-Sr等时线定年的可靠性.地球化学,30(6):507~511.
於崇文,岑况,鲍征宇.1998.成矿作用动力学.北京:地质出版社:1~224.
岳文浙,魏乃甄,焦世鼎.1993.长江中下游威宁期沉积地质与块状硫化物矿床.北京:地质出版社,50~78.
臧文拴,吴淦国,张达,刘爱华.2004.铜陵新桥铁矿田地质地球化学特征及成因浅析.大地构造与成矿学,28(2):187~193.
翟伟,李兆麟,黄栋林,文拥军.2004.粤西河台金矿床富硫化物石英脉Rb-Sr等时线年龄讨论.地球学报,25(2):2443~247.
翟裕生,姚书振,林新多,金福全,周珣若,万天丰,周宗桂.1992.长江中下游地区铁、铜等成矿规律研究.矿床地质,11(1):1~235.
张德贵.1982.安徽最大铜硫矿床地质概要——论新桥铜硫铁矿床的成因.地质科技情报,(S1):73~75.
张宇.201 1.安徽铜陵新桥铜硫铁矿床地质地球化学特征及矿床成因分析.导师:邵拥军.长沙:中南大学地球科学与信息物理学院硕士学位论文:1~98.
张宇,邵拥军,周鑫,刘忠法,郑明泓.2013.安徽铜陵新桥铜硫铁矿床胶状黄铁矿主、微量元素特征.中国有色金属学报,23(12):3492~3502.
郑培玺,周燕,王铁夫,张延洁.2007.山东招远灵雀山金矿床富金石英脉铷-锶等时线年龄讨论.岩矿测试,26(5):356~358.
周强强,胡文洁.2012.Sr同位素的研究现状和最新进展.科技信息,1:396.
周涛发,范裕,袁峰.2008.长江中下游成矿带成岩成矿作用研究进展.岩石学报,24(8):1665~1678.
周涛发,岳书仓.2000.长假中下游两个系列铜金矿床成矿流体系统的形成条件及机理.北京大学学报(自然科学版),36(5):697~707.
周涛发,张乐骏,袁峰,范裕,David R.Cooke.2010.安徽铜陵新桥Cu—Au—S矿床黄铁矿微量元素LA-ICP-MS原位测定及其对矿床成因的制约.地学前缘,17(2):306~319.
Cu Lianxing,Hu Wenxuan,He Jinxiang,Ni Pei,Xu Keqin.2000.Regional variations in ore composition and fluid features of massive sulfide deposits in South China:Implications for genetic modeling.Episodes,23(2):110~118.
John F S,Julie A D,Jeanine M S,Lorn E E Y,Cameron S R.Paleozoic sedimentary rocks in the Red Dog Zn—Pb—Ag district and Vicinity,Western Brooks Range,Alaska:Provenance,deposition and metallogenic significance for the genesis of the orebodies.Economic Geology,2004,99(7):1385~1414.
Ludwing K R.2001.ISOPLOT/Ex.Version 2.49.A Geochronological Toolkit for Microsoft Excel.Berkeley Geochronology Center,1~20.
Mao Jingwen,Xie Guiqing,Duan Chao,Franco Pirajno,Dazio Ishiyama,Chen Yuchuan.2011.A Tectono-Genetic Model for Porphyry-Skarn-Stratabound Cu—Au—Fe and Magnetite—Apatite Deposit Along the Middle—Lower Yangtze River Valley,Eastern China.Ore Geology Reviews,2011,43(1):294~314.
Pan Yuanming,Done Ping.1999.The lower Changjiang(Yangtzi/Yangtze River)metallogenic belt,east—center China:intrusion and wall rock hosted Cu—Fe—Au,Mo,Zn,Pb,Ag deposits.Ore Geology Reviews,15(4):177~242.
Pettke T,Diamond L W.1995.Rb-Sr isotopic analysis of fluid inclusions in quartz.-Evaluation of bulk extraction procedure and geochronometer systematics using synthetic fluid inclusions.Geochimica et Cosmochimica Acta,59:4009~4027.
Rossman G R,Weis D,Wasserburg G J.1987.Rb,Sr,Nd and Sm concentrations in quartz.Geochmiica et Cosmochmiica Acta,51:2325~2329.
Shepherd T J,Darbyshire D P E.1982.Fluid inclusion Rb-Sr isochrones for dating mineral deposits.Narture,1981,290:578~579.
Wang Yue,Zhu X iangkun,Mao Jingwen,Li Zhihonh,Cheng Yanbo.2011.Iron Isotope Fractionation During Skarn-Type Metallogeny:A Case Study of Xiao Cu—S—Fe—Au Deposit in the Middle—Lower Yangtze Valley.Ore Geology Reviews,43:194~202.
Xu G,Zhou J.2001.The Xinqiao Cu—S—Fe—Au deposit in the Tongling mineral district,China:synorogenic remobilization of a stratiform sulfide deposit.Ore Geology Reviews,18:77~94.