| 胶东及小秦岭金矿成矿期流体成分对比研究 |
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| 引用本文： | 李力,郑超.胶东及小秦岭金矿成矿期流体成分对比研究[J].黄金,1991,12(9):1-5. |
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| 作者姓名： | 李力 郑超 |
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| 作者单位： | 沈阳黄金学院
(李力，郑超，毛冬青)，沈阳黄金学院(于志凯) |
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| 摘 要： | 通过对胶东,小秦岭两大金矿产区典型金矿床中成矿期流体成分对比的研究,结合地质特征,得出了胶东金矿床成矿流体与花岗侵入作用有关,小秦岭金矿区矿床成矿流体与变质热液有密切联系的结论,并从流体成分的演化特点推定:胶东金矿有迭加成矿的可能。并对两矿区成矿物质可能存在的迁移方式做了设想。
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| 关 键 词： | 胶东矿 小秦岭 金矿 成流体 |
To contrast the fluid composition in mineralizing period in the Gold Field of Jiao-Dong with that in Xiao-Qin-Ling Gold Field |
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| LiLi et al..To contrast the fluid composition in mineralizing period in the Gold Field of Jiao-Dong with that in Xiao-Qin-Ling Gold Field[J].Gold,1991,12(9):1-5. |
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| Authors: | LiLi |
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| Affiliation: | Shenyang Gold College |
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| Abstract: | Based on the geological feature and the contrast of fluid composition in mineralizingperiod of the typical gold deposits in Jiao-Dong Gold Field with that in Xiao-Qin-Ling,it is concluded that the mineralizing fluid of Jiao Dong Gold Deposits is related to the granitic intrusion,while Xiao-Qin-Ling Gold Deposits is closely related to the metamorphic hydrothermal fluid.Based on the characteristics of the evolution of fluid composition, it is inferred that Jiao-Dong Gold Deposit is probably of superimposed mineralization.The possible migrational modes of the mineralizing materials in the two fields are inferred. |
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| Keywords: | Jiao-Dong Xiao-Qin-Ling mineralizing fluid migrational mode |
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