| 新疆托里齐求Ⅰ号金矿控矿构造研究 |
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| 引用本文： | 荆福建.新疆托里齐求Ⅰ号金矿控矿构造研究[J].资源调查与环境,2000(1). |
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| 作者姓名： | 荆福建 |
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| 作者单位： | 南京地质矿产研究所!南京210016 |
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| 摘 要： | 齐求Ⅰ号金矿产于中晚石炭统海相基性火山喷发沉积岩中 ,为典型的中温热液矿床 ,以石英脉型金矿为主 ,蚀变岩型金矿为辅。矿化受断裂控制 ,系火山机构与断裂构造复合控矿 ,环状构造内北西向断裂矿化较好 ,矿脉向西南深部有归并趋势。
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| 关 键 词： | 火山机构 复合控矿 |
ORE-FIELD TECTONICS OF QIQIU-1 GOLD DEPOSIT IN TUOLI,XINJIANG |
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| Jing Fujian.ORE-FIELD TECTONICS OF QIQIU-1 GOLD DEPOSIT IN TUOLI,XINJIANG[J].Resources Survey & Environment,2000(1). |
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| Authors: | Jing Fujian |
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| Abstract: | Qiqiu-1 Gold Deposit in Tuoli, Xinjiang province,occured in the marine basic volcanic-sedimentary rocks of middle and upper Carboniferous, and it is typical of mesothermal deposit. Its ore-types consists of quartz vein and altered rocks and the former is of more important,strictly controlled or defined by faults and volcanic mechanism. The mineralization is much better in the NW faults occuring in the ring fracture.The lodes in ring fracture converged to depth of southwest. |
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| Keywords: | volcanic apparatus polygenetic ore-controlling |
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