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若羌县亚干布阳萤石矿地质特征及成因分析

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亚干布阳萤石矿位于阿中地块南部的三级构造单元——阿尔金杂岩带中南部,属阿尔金(地块)Fe-Cu-Ni-萤石-石棉-玉石-白云母-白云岩-石英岩-石膏-煤矿带.萤石矿化主要分布于盖吉勒断裂两侧的阿尔金岩群a岩组黑云斜长片麻岩地层、中奥陶世侵入岩及方解石脉发育地段,明显受地层、岩性、断裂等因素控制.初步研究认为,矿床成因类型为低温热液充填型萤石矿床.
Analysis on Geological Characteristics and Genesis of the Yaganbuyang Fluorite Deposit in Ruoqiang County
The Yaganbuyang Fluorite Deposit is located in the central southern part of the Altun Complex,a tertiary tectonic unit in the southern part of the Azhong Block,it belongs to the Altun(massif)Fe-Cu-Ni-fluorite-asbestos-jade-muscovite-dolomite-quartzite-gypsum-coal ore belt.Fluorite mineralization is mainly distributed in the biotite plagioclase gneiss strata of a rock group of the Altun rock group on both sides of the Gaijile fault,as well as in the areas where Middle Ordovician intrusive rocks and calcite veins are developed,it is clearly controlled by factors such as strata,lithology,and faults.Preliminary research suggests that the genesis type of the deposit is a low-temperature hydrothermal filled fluorite deposit.

Yaganbuyang Fluorite Depositgeological characteristicsgenesisRuoqiang County

汪东、李月栋、连政

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新疆地质矿产勘查开发局第一区域地质调查大队,乌鲁木齐 830013

亚干布阳萤石矿 地质特征 成因 若羌县

2024

中国资源综合利用
徐州北矿金属循环利用研究所 中国物资再生协会

中国资源综合利用

CHSSCD
影响因子:0.358
ISSN:1008-9500
年,卷(期):2024.42(2)
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