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论接触交代矽卡岩型多金属矿床的矿质来源—以铅同位素组成为依据
引用本文:张乾,潘家永.论接触交代矽卡岩型多金属矿床的矿质来源—以铅同位素组成为依据[J].矿物学报,1994,14(4):369-372.
作者姓名:张乾  潘家永
作者单位:中国科学院地球化学研究所!贵阳,550002,中国科学院地球化学研究所!贵阳,550002
摘    要:本文以铅同位素组成为线索,讨论了与中酸性侵入岩有关的接触交代矽卡岩型铜铅锌多金属矿床的矿质来源,得出了该类矿床矿质的岩浆源、岩浆与围岩混合源及多源混合源三种来源。

关 键 词:矽卡岩型多金属矿床  铅同位素组成  矿质来源

SOURCES OF ORE-FORMING MATERIALS OF THE CONTACTMETASOMATIC SKARN-TYPE Cu-Pb-Zn DEPOSITS IN SPECIAL REFERENCE TO THEIR LEAD ISOTOPIC COMPOSITON
Zhang Qian, Pan Jiayong.SOURCES OF ORE-FORMING MATERIALS OF THE CONTACTMETASOMATIC SKARN-TYPE Cu-Pb-Zn DEPOSITS IN SPECIAL REFERENCE TO THEIR LEAD ISOTOPIC COMPOSITON[J].Acta Mineralogica Sinica,1994,14(4):369-372.
Authors:Zhang Qian  Pan Jiayong
Abstract:As viewed from a traditional consideration, ore-forming materials of the contact-metasomaticskarn-type Cu-Pb-Zn deposits are derived from magmatic differentiation. In this paper, based onthe comparison of ore lead isotopes with those of magmatic rocks and country rocks,the authorsproposed three types of ore-forming material sources for these deposits, i. e-, magmatic source,mixing source (magma and country rock)and multiple mixing source.
Keywords:skarn-type deposit  lead isotopic composition  ore-forming material source
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