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安徽省许村金矿矿床地质特征及找矿远景分析

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本区大地构造位置处于扬子准地台下扬子台坳的石台穹褶断束与江南台隆交接部位,地质发展历史悠久,地质构造复杂.自中元古以来,经历了多次构造运动,各时代地层均发生了不同程度的褶皱,其中以印支期最为强烈,构成了北东东向展布的构造格架.断裂构造十分发育,该区金银铜铅锌等矿产资源丰富,成矿条件优越.
Geological characteristics and prospecting prospect analysis of Xucun gold deposit in Anhui Province
The geological structure of this area is located at the junction of Shitai dome fold fault bundle and Jiangnan Terrace rise under the Yangtze penestrum,which has a long geological development history and complex geological structure.Since the Middle Proterozoic,it has experienced many tectonic movements,and the strata of all ages have different degrees of folding,among which the Indosinian period is the most intense,forming a tectonic framework spreading in the direction of northeast to east.The fault structure is very developed,the area is rich in gold,silver,copper,lead and zinc and other mineral resources,metallogenic conditions are superior.

Gold depositGeological characteristicsProspecting prospect

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池州市贵池区自然资源和规划局,安徽 池州 247000

金矿床 地质特征 找矿远景

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.(2)
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