| 新疆中天山胜利达坂金矿区花岗质岩石中金的分形研究 |
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| 引用本文： | 刘养杰,王焰.新疆中天山胜利达坂金矿区花岗质岩石中金的分形研究[J].西北大学学报,1995,25(6):697-700. |
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| 作者姓名： | 刘养杰 王焰 |
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| 作者单位： | 西北大学地质学系 |
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| 基金项目： | 国家三零五项目：85－902－04－04资助课题 |
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| 摘 要： | 用分形理论研究了胜利达圾金矿区花岗质岩石中金含量的分布特征，得出花岗质岩石的金是在韧性剪切活动中被激化的。一部分金被迁移至相邻的黄铁矿化的花岗质糜棱岩中，所构成的金矿（化）体规模大，但金品位低，与围岩没有明显的界线；而另一部分金则被迁移至其他的岩石中去。
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| 关 键 词： | 分形结构因子（FSF） 金含量 花岗质岩石 新疆胜利达坂 |
Fractal Study of Au in Granitic Rocks from Au Mineralized District of Shenglidaban,Xinjiang Autonomous Region |
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| Liu Yangjie,Wang Yan,Wang Juli,Wang Runsan,Yan Jincai.Fractal Study of Au in Granitic Rocks from Au Mineralized District of Shenglidaban,Xinjiang Autonomous Region[J].Journal of Northwest University(Natural Science Edition),1995,25(6):697-700. |
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| Authors: | Liu Yangjie Wang Yan Wang Juli Wang Runsan Yan Jincai |
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| Abstract: | The distributive characters of Au content in granitic rocks from Au mineralized district inShenglidaban has been studied with fractal theory,The study indlcates that, during ductile shearactiveity,certain part of Au orebodies formed in this way is usually in large-scale,but Au grade isrelatively low and there is no distinct boundary between the orebody and its country rocks.Anotherpart of Au,however,is migrated to other orebodies. |
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| Keywords: | fractal structure factor(FSP) Au content granitic rocks Shenglidaban Xinjiang |
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