华南地质与矿产
華南地質與礦產
화남지질여광산
GEOLOGY AND MINERAL RESOURCES OF SOUTH CHINA
2012年
2期
175-180
,共6页
硫化物矿床%闪锌矿%Rb-Sr等时线定年%湘西,新晃打狗洞
硫化物礦床%閃鋅礦%Rb-Sr等時線定年%湘西,新晃打狗洞
류화물광상%섬자광%Rb-Sr등시선정년%상서,신황타구동
sulphide mineral deposit%Sphalerite%Rb-Sr isochrone dating%Dagoudong deposit,Xinhuang county,western Hunan province
本文对用研磨法和分步溶解技术提取流体相和硫化物相的实验条件进行了系统的研究,在此基础上建立和完善了闪锌矿分相Rb-Sr等时线定年的方法流程。通过对湘西打狗洞铅锌矿床Rb-Sr定年的示范研究,进一步验证了方法的有效性和应用前景,获得闪锌矿矿物Rb-Sr等时线年龄(473±76 Ma),采用研磨法和分步溶解技术获得更精确的闪锌矿流体相+硫化物相年龄(489.6±5.9 Ma)和全矿物+矿物相(流体相+硫化物相)的年龄(490±6.5 Ma),表明湘西打狗洞铅锌矿床的成矿作用发生在早奥陶世,其成矿作用的发生可能与晚期成岩或区域构造热事件有关。
本文對用研磨法和分步溶解技術提取流體相和硫化物相的實驗條件進行瞭繫統的研究,在此基礎上建立和完善瞭閃鋅礦分相Rb-Sr等時線定年的方法流程。通過對湘西打狗洞鉛鋅礦床Rb-Sr定年的示範研究,進一步驗證瞭方法的有效性和應用前景,穫得閃鋅礦礦物Rb-Sr等時線年齡(473±76 Ma),採用研磨法和分步溶解技術穫得更精確的閃鋅礦流體相+硫化物相年齡(489.6±5.9 Ma)和全礦物+礦物相(流體相+硫化物相)的年齡(490±6.5 Ma),錶明湘西打狗洞鉛鋅礦床的成礦作用髮生在早奧陶世,其成礦作用的髮生可能與晚期成巖或區域構造熱事件有關。
본문대용연마법화분보용해기술제취류체상화류화물상적실험조건진행료계통적연구,재차기출상건립화완선료섬자광분상Rb-Sr등시선정년적방법류정。통과대상서타구동연자광상Rb-Sr정년적시범연구,진일보험증료방법적유효성화응용전경,획득섬자광광물Rb-Sr등시선년령(473±76 Ma),채용연마법화분보용해기술획득경정학적섬자광류체상+류화물상년령(489.6±5.9 Ma)화전광물+광물상(류체상+류화물상)적년령(490±6.5 Ma),표명상서타구동연자광상적성광작용발생재조오도세,기성광작용적발생가능여만기성암혹구역구조열사건유관。
This paper takes a systematic study on the experimental conditions using the grinding method and stepping dissolution technique to extract the fluid phase and sulfide phase from sphalerite for Rb-Sr isochrone dating,and the entire analysis process was established and improved.Through the demonstration of Rb-Sr dating method used in Dagoudong Pb-Zn deposits,western Hunan,the validity of the method was further verified and showed a good application prospects.Three isochron ages are obtained:473±76 Ma for sphalerite mineral-phase,489.6±5.9 Ma for fluid phase +sulfide phase of sphalerite by grinding method and stepping dissolution technique,490±6.5 Ma for mineral-phase and fluid phase +sulfide phase of sphalerite.The isochron ages indicated that Dagoudong deposit was formed in Early Ordovician,and maybe related to later diagenesis or regional tectono-thermal events.