厘定矿床的形成时代对于正确认识矿床的成因、了解成矿机制和控矿因素以及掌握成矿规律并指导进一步找矿勘查具有重要意义.与热液有关的金矿床由于成矿热液来源的复杂性以及多期性,确定其矿化发生的年代一直是矿床学研究中的难点.对与热液金矿成矿同时形成的单矿物甚至载金矿物进行同位素直接定年,能够得到与热液成矿有关的金矿床的形成年代.对于单个矿床而言,应该根据相应的成岩成矿地质背景选择合适的定年矿物以及放射性同位素定年体系进行成矿年代的测定,得到具有地质意义的成矿年龄.在前人研究的基础上,对当前确定与热液成矿有关的金矿床成矿时代中应用最广泛有效的几种定年方法技术进行简要评述.
参考文献
[1] | 魏俊浩,刘丛强,刘国春.金矿测年方法讨论及定年中存在的问题[J].地学前缘,2003(02):319-326. |
[2] | Hu Ruizhong;Turner G;Bumard P G et al.Helium and argon isotope geochemistry of Jingding supper large Pb-Zn deposit[J].Science in China(Series D),1998,41(04):442-448. |
[3] | Kelley S;Turner G;Buttwefield A W et al.The source and significance of argon isotopes of fluid inclusion from areas of mineralization[J].Earth and Planetary Science Letters,1986,19:303-318. |
[4] | 邱华宁;李朝阳 .滇西芒岗金矿石英流体包裹体成矿年龄测定[J].科学通报,1994,39(03):257-260. |
[5] | 赵羽军,崔培龙,王清海,孙景贵,郭佳.黑龙江宁安英城子热液金矿床流体包裹体的氩同位素激光探针定年与成矿时代讨论[J].世界地质,2010(02):203-210. |
[6] | 于介江,郭佳,崔培龙.延边海沟金矿床石英流体包裹体激光探针40Ar/39Ar测年与成矿背景[J].吉林大学学报(地球科学版),2010(04):835-844. |
[7] | Harrison T M;Aleinkoff J N;Compston W .Observation and controls on the occurrence of inherited zircon in concord-type granitoids,New Hampshire[J].GeochimicaetCosmochimicaActa,1987,51:2549-2568. |
[8] | Tilton G R;schreyer W;schertl H P .Pb-Sr-Nd isotopic behavior of deeply subducted crustal rocks from the Dora Maira massif,Western Alps,Italy:What is the age of the ultra-high pressure metamorphism[J].Contribution to Mineralogy Petrology,1991,108:22-23. |
[9] | Mezger K;Krogstad E J .Interpretation of discordant U-Pb zircon ages:An evaluation[J].Journal of Metamorphic Geology,1997,15:127-140. |
[10] | Claoue-Long J C;King R W;Kerrich R .Archaean hydrothermal zircon in the Abitibi greenstone belt:Constraints on the timing of gold mineralisation[J].Earth and Planetary Svience Letters,1990,98(01):109-128. |
[11] | Rubin J N;Henry C D;Price J G .The mobility of zirconium and other "immobile" elements during hydrothermal alteration[J].Chemical Geology,1993,110(1-3):29-47. |
[12] | Hoskin P W O;Kinny P D;Wyborn D.Chemistry of hydrothermal zircon:investigating biming and nature of water-rock interaction[A].Rotterdam:Balkema,1998:545-548. |
[13] | HU Fangfang,FAN Hongrui,YANG Jinhui,WAN Yusheng,LIU Dunyi,ZHAI Mingguo,JIN Chengwei.Mineralizing age of the Rushan lode gold deposit in the Jiaodong Peninsula: SHRIMP U-Pb dating on hydrothermal zircon[J].科学通报(英文版),2004(15):1629-1636. |
[14] | Dubinska E.;Bylina P.;Kozlowski A.;Dorr W.;Nejbert K.;Schastok J. Kulicki C. .U-Pb dating of serpentinization: hydrothermal zircon from a metasomatic rodingite shell (Sudetic ophiolite, SW Poland) [Review][J].Chemical geology,2004(3-4):183-203. |
[15] | 吴元保,郑永飞.锆石成因矿物学研究及其对U-Pb年龄解释的制约[J].科学通报,2004(16):1589-1604. |
[16] | 朱永峰,宋彪.新疆天格尔糜棱岩化花岗岩的岩石学及其SHRIMP年代学研究:兼论花岗岩中热液锆石边的定年[J].岩石学报,2006(01):135-144. |
[17] | Hoskin PWO .Trace-element composition of hydrothermal zircon and the alteration of Hadean zircon from the Jack Hills, Australia[J].Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society,2005(3):637-648. |
[18] | Schaltegger U .Hydrothermal zircon[J].Elements,2007,3(01):51-52. |
[19] | 毕诗健,李建威,赵新福.热液锆石U-Pb定年与石英脉型金矿成矿时代:评述与展望[J].地质科技情报,2008(01):69-76. |
[20] | Liati A;Gebauer D .Constraining the pregrade and regrade P-Tt path of Eocene HP rocks by SHRIMP dating difference zircon domain:Inferred rated of heating-burial,cooling and exhumation for central Rhodope,northern Greece[J].ContribMinem Petrol,1999,135:340-354. |
[21] | Vavra G;Gebauer D;Schmid R .Multiple zircon growth and recrystallization during polyphase Late Carboniferous to Triassic metamorphism in granulites of the Ivrea Zone (Southern Alps):An ion microprobe (SHRIMP) study[J].Contributions to Mineralogy & Petrology,1996,122:337-358. |
[22] | Schaltegger U;Fanning C M;Gunther D et al.Growth,annealing and recrystllization of zircon and preservation of monazite in high-grade metamorphism:Conventional and in-situ U-Pb isotope,cathodoluminescence and microchemical evidence[J].Contributions to Mineralogy & Petrology,1999,134:186-201. |
[23] | Liati A.;Gebauer D.;Wysoczanski R. .U-Pb SHRIMP-dating of zircon domains from UHP garnet-rich mafic rocks and late pegmatoids in the Rhodope zone (N Greece); evidence for Early Cretaceous crystallization and Late Cretaceous metamorphism[J].Chemical geology,2002(3-4):281-299. |
[24] | 李长民,邓晋福,陈立辉,苏尚国,李惠民,胡森林,刘新秒.华北北缘张宣地区东坪金矿中的两期锆石:对成矿年龄的约束[J].矿床地质,2010(02):265-275. |
[25] | Faure G.Principles of Isotope Geology[M].New York:Wi1ey,1986:117-140. |
[26] | 陈光远;邵伟;孙岱生.胶东金矿床成因矿物学与找矿[M].重庆:重庆大学出版社,1989 |
[27] | Barton E S;Hallbauer D K .Trace-element and U-Pb isotope compositions of pyrite types in the Proterozoic Black Reef,Transvaal Sequence,South Africa:Implications on genesis and age[J].Chemical Geology,1996,133:173-199. |
[28] | Volker Luders;Martin Ziemann .Possibilities and limits of infrared light microthermometry applied to studies of pyrite-hosted fluid inclusions[J].Chemical geology,1999(1/4):169-178. |
[29] | 毛光周,华仁民,高剑峰,龙光明,陆慧娟.江西金山金矿含金黄铁矿的Rb-Sr年龄[J].地球学报,2008(05):599-606. |
[30] | 杨进辉,周新华.胶东地区玲珑金矿矿石和载金矿物Rb-Sr等时线年龄与成矿时代[J].科学通报,2000(14):1547-1553. |
[31] | 韩以贵,李向辉,张世红,张元厚,陈福坤.豫西祁雨沟金矿单颗粒和碎裂状黄铁矿Rb-Sr等时线定年[J].科学通报,2007(11):1307-1311. |
[32] | 卿敏,葛良胜,唐明国,屈文俊,袁士松,赵玉锁.内蒙古苏尼特右旗毕力赫大型斑岩型金矿床辉钼矿Re-Os同位素年龄及其地质意义[J].矿床地质,2011(01):11-20. |
[33] | 谢智;陈江峰 .Re-Os同位素体系在金属矿床研究中的应用[J].地质地球化学,1998,26(04):79-85. |
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