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云南会泽铅锌矿喷流沉积成因研究
引用本文:李家盛,李采一,崔银亮,杨灿.云南会泽铅锌矿喷流沉积成因研究[J].云南地质,2005,24(3):254-263.
作者姓名:李家盛  李采一  崔银亮  杨灿
作者单位:云南省有色地质勘查院,昆明,650216
摘    要:会泽铅锌矿床的成因认识各异,曾认为是沉积—改造层控型矿床。研究前人资料、结合亲历找矿实践,讨论该矿床另一种不同的成矿方式。研究矿床地质、地球化学、同位素组成、包裹体、方铅矿年龄测定和成矿温度测试等表明:会泽铅锌矿属海底热卤水喷流沉积—改造层控型矿床,与芒特—艾萨型热卤水喷流沉积层控矿床类似。

关 键 词:热卤水  喷流沉积  改造层控  铅锌矿  会泽云南
文章编号:1004-1885(2005)03-254-10
收稿时间:2003-01-15
修稿时间:2003-01-15

A STUDY ON THE EFFUSIVE SEDIMENTARY GENESIS OF HUIZE PB- ZN DEPOSIT, YUNNAN
LI Jia-sheng,LI Cai-yi,CUI Yin-liang,YANG Can.A STUDY ON THE EFFUSIVE SEDIMENTARY GENESIS OF HUIZE PB- ZN DEPOSIT, YUNNAN[J].Yunnan Geology,2005,24(3):254-263.
Authors:LI Jia-sheng  LI Cai-yi  CUI Yin-liang  YANG Can
Institution:Yunnan Nonferrous Geological Survey, Kunming 650216
Abstract:There are various viewpoints on the genesis of the famous Huize Pb-Zn deposit in Dian-Chuan-Qian metallogenetic province, which has been regarded as a sedimentation-reformation stratabound deposit. According to the study on previous materials in combination with the ore-prospecting practice by ourselves, we provide ample evidence for another metallogene tic model of this ore deposit. The study on the characteristics of geology, geochemistry of ore deposit, isotopic composition and inclusion of mineral and the galena dating, metallogenetic temperature testing shows that the Huize Pb-Zn deposit belongs to the submarine hot brine effusive sediment tion-reformation stratabound deposit.
Keywords:Hot Brine  Effusive Sedimetation  Genesis of Ore Deposit  Huize Pb-Zn Deposit Yunnan
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