申萍.陕西镇安丘岭微细浸染型金矿床同位素组成特征及成因意义[J].地质找矿论丛,1996,(4):27-34
陕西镇安丘岭微细浸染型金矿床同位素组成特征及成因意义
ISOTOPIC COMPOSITIONS IN THE QIULING MICRODISSEMINATED GOLD DEPOSIT, ZHEN'AN COUNTY, SHANXI PROVINCE, AND THEIR GENETIC IMPLICATIONS
投稿时间:1996-07-15  
DOI:10.6053/j.issn.1001-1412.1996.4. 003
中文关键词:  同位素  微细浸染型金矿  丘岭
英文关键词:
基金项目:
作者单位
申萍 西安矿业学院地质系 
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中文摘要:
      本文通过硫、氢、氧、碳、铅同位素组成的研究,认为成矿溶液来自大气降水,成矿物质来自南羊山组和袁家沟组的不纯细碎屑岩-碳酸盐岩。在此基础上分析了成矿过程。
英文摘要:
      This paper presents S, H, O, C isotopic data obtained from Qiuling micro-fine disseminated gold deposit. H2O in.ore fluid is mainly from ancient meteoric water. Ore-forming materials are dominated by those derived from impure-fine clasitic carbonate rock of Nanyangshan Formation and Yuanjiagou Formation. Then ore-forming processes are analysed.
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