辽吉裂谷区铅锌金矿床S、Pb同位素组成特征及其地质意义
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国家自然科学基金青年基金项目(编号:41202042)、中央级公益性科研院所基本科研业务费专项资金资助项目(编号:K1211)和中国地质调查局地质矿产调查评价专项项目(编号:1212011085530)


Sulfur, Lead Isotope Comoposition Characteristics and the Geological Significance of the Polymetallic Deposits in Liao-ji Rift
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    摘要:

    辽吉裂谷区发育有众多大中型铅锌、金等多金属矿床,本文选择该地区的青城子榛子沟铅锌矿、白云金矿、五龙金矿、荒沟山铅锌矿和临江金矿作为研究对象,开展其矿石S、Pb同位素分析及其地质意义研究。数据显示榛子沟脉状铅锌矿δ34SCDT值介于-10.3‰~6.8‰之间,白云金矿δ34SCDT值介于-7.7‰~1.9‰之间,五龙金矿δ34SCDT值介于0.8‰~3.6‰之间,荒沟山铅锌矿δ34SCDT值介于6.7‰~17.8‰之间,临江金矿δ34SCDT值介于0.7‰~1.5‰之间。研究区铅锌金矿床的矿石硫同位素主要有两种来源,其一来自于早期火山喷流沉积而成的地层硫,如青城子榛子沟层状铅矿矿体和荒沟山层状铅锌矿;另一类为后期岩浆硫,如青城子榛子沟脉状铅锌矿、白云金矿、五龙金矿以及临江金矿,此类岩浆硫形成过程中,对早期地层硫进行了混染。辽吉裂谷区典型多金属矿床矿石铅同位素值变化较大,206Pb/204Pb值介于15.72~24.02,207Pb/204Pb值介于15.32~16.43,208Pb/204Pb值介于34.96~39.79,不同的矿床其比值具有不同特点。研究区铅同位素μ值相对集中且较大,显示铅源具有上地壳物质特征,但均受到了不同铅源的混合。榛子沟铅锌矿脉状矿体矿石铅和岩体铅均为混合铅源,矿石铅为上地壳与地幔的混合源铅,而岩体铅则是造山带铅与上地壳的混合源铅;白云金矿床矿石铅为造山带铅,而其岩体铅为上地壳与地幔的混合源铅;五龙金矿的铅同位素主要来源于元古代造山带铅,同时又有幔源铅的混合;荒沟山铅锌矿矿石铅一组为正常铅,微偏钍铅,来源于统一矿源层,另外一组铅为放射成因铅,即铀铅,而临江金矿矿石铅属于放射成因铅。

    Abstract:

    Plenty of Pb-Zn, Au polymetallic deposits developed in Liao-ji rift, and this study choose Zhenzigou Pb-Zn deposit in Qingchengzi, Baiyun Au deposit, Wulong Au deposit, Huanggoushan Pb-Zn deposit and Linjiang Au deposit as the objects of the research to analysis the sulfur, lead isotope and its geological significance. The results show that the δ34SCDT values of Zhenzigou veined Pb-Zn vary from -10.3‰~6.8‰, the δ34SCDT values of Baiyun Au deposit vary from -7.7‰~1.9‰, the δ34SCDT values of Wulong Au deposit vary from 0.8‰~3.6‰, the δ34SCDT values of Huanggoushan Pb-Zn deposit vary from 6.7‰~17.8‰, the δ34SCDT values of Linjiang Au deposit vary from 0.7‰~1.5‰. Two sulfur source exist in polymetallic deposit in Liao-ji rift: one of the type is formation sulfur and the other type is magmatic sulfur. Layered ore body of Zhenzigou Pb-Zn deposit belong to the first type, and the sulfur in veined Pb-Zn ore body, Baiyun Au deposit, Wulong Au deposit and Linjiang Au deposit belong to de later type. The formation sulfur aways contamined by the later magmatic sulfur. The Pb isotope from these deposits varied greatly. The 206Pb/204Pb, 207Pb/204Pb and 208Pb/204Pb range respectively within 15.32~16.43, 15.72~24.02 and 34.96~39.79, while every deposit had its own characters. The μvalue of ore lead isotope of the study objects are relative concentrated and high, show upper crust lead source and contamined by different other type lead isotope. Lead isotope of veined Pb-Zn ore body and rock body in Zhenzigou are mixed lead, while lead of veined ore body lead is mixed by upper crust lead and mantle lead, the lead of rock body is mixed by orogenic belt lead and upper crust lead. Ore lead of Baiyun Au deposit is orogenic belt lead, while rock body lead is mixed by upper crust lead and mantle lead. Lead isotope of Wulong Au deposit is mainly orogenic belt lead and contamined by mantle lead. Two lead types developed in Huanggoushan Pb-Zn deposit, one type is normal lead, which contain slightly more thorium and mainly from unite source bed. The other type is radiogenic lead (Uranium lead), and ore lead of Linjiang Au deposit belong to this type.

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马玉波,邢树文,张增杰.2013.辽吉裂谷区铅锌金矿床S、Pb同位素组成特征及其地质意义[J].地质学报,87(9):1399-1410.
mayubo, xingshuwen, zhangzengjie.2013. Sulfur, Lead Isotope Comoposition Characteristics and the Geological Significance of the Polymetallic Deposits in Liao-ji Rift[J]. Acta Geologica Sinica,87(9):1399-1410.

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  • 收稿日期:2013-06-03
  • 最后修改日期:2013-08-07
  • 录用日期:2013-08-08
  • 在线发布日期: 2013-09-13
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