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甘肃唐坝金矿地质特征与矿床成因浅析

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本文通过对甘肃唐坝地区开展金矿勘查工作,在介绍唐坝金矿成矿地质背景的基础上,详细描述了该地区金矿的矿床成因,认为形成唐坝金矿的成矿流体主要为区域断裂形成的构造热液,受纵弯褶皱作用,成矿流体在中厚层灰岩下部富集成矿,金矿体产于复式背(向)斜转折端形成的虚脱部位和层间滑脱构造面,矿体形态呈鞍状、似层状、透镜状、网脉状.矿石类型主要为石英脉型,矿化主要为褐铁矿化、黄铁矿化、硅化;围岩蚀变主要为绿泥石化、绢云母化.
Geological characteristics and genetic analysis of Tangba gold deposit in Gansu Province
In this paper,the gold deposit genesis of Tangba gold deposit in Gansu Province is described in detail on the basis of the introduction of the geological setting of Tangba gold deposit.It is believed that the ore-forming fluid of Tangba gold deposit is mainly acidic tectonic hydrothermal fluid formed by regional faults,and the ore-forming fluid is enriched in the lower part of the middle-thick limestone due to longitudinal bending and folding.The gold ore body is located at the collapse site and the interlayer slip tectonic plane formed by the complex back(toward)inclined turning point,and the ore body shape is saddle-like,lamellar,lens-like,and netted.The ore type is mainly quartz vein type,and the mineralization is mainly limonite,pyrite and silicitization.The alteration of surrounding rock is mainly chlorite and sericite.

Tangba gold mineComplex anticlinebucklingstructural hydrothermal

张海宝

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甘肃省有色金属地质勘查局兰州矿产勘查院,甘肃 兰州 730000

唐坝金矿 复式背斜 纵弯褶皱作用 构造热液

甘肃省自然资源厅"甘肃省陇南市赵家沟金矿普查"项目

202202-Y06

2024

世界有色金属
有色金属技术经济研究院

世界有色金属

影响因子:0.138
ISSN:1002-5065
年,卷(期):2024.(15)
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