摘要
研究表明灵雀山金矿硫同位素组成为:δ^34S值为6.6‰~10.4‰,平均值为7.9‰。矿石铅同住素组成为:206Pb/204Pb为17.114~17.774,平均17.467;207Pb/204Pb为15.451~15.566,平均15.508;208Pb/204Pb为36.917~38.737,平均37.870。与其赋矿围岩的同位素组成不同。这说明该矿床的成矿物质可能部分来自幔源,具有与招掖金矿带其它金矿类似的特征。
Sulfur isotope analyses show that δ34S values of pyrites vary in the range of 6.6‰-10. 40‰, with an average of 7.9‰. Pb isotope analyses show that 206Pb/204pb, 2207Pb/204pb and 2208Pb/204pb rations of the ore lend are 17.114-17. 774, 15.451- 15. 566,36. 917-38. 737, and with an average of 17. 467, 15. 508 and 37. 870 respectively, which are significantly different from the data of granites. The research results show that ore-forming materials of the Lingqueshan gold Deposit might have partly derived from the mantle, and the geochemial characteristics are similar to the Zhao-Ye gold zone one.
出处
《吉林地质》
2006年第1期12-16,共5页
Jilin Geology
关键词
灵雀山金矿
硫同位素
铅同位素
物质来源
Lingqueshan gold deposit isotopes Pb isotopes material sources