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晋东北地区金矿成矿控矿因素的物化探特征

THE GEOPHISICAL AND GEOCHEMICAL FEATURES OF ORE-CONTROLLING FACTORS FOR GOLD DEPOSITS IN NORTHEASTERN SHANXI PROVINCE
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摘要 本文利用地质、物化探、遥感资料综合分析了晋东北地区金矿的控矿因素。早前寒武纪结晶基底与金成矿关系密切,五台超群中的含铁建造是重要的金矿源层。利用断裂构造原生晕和元素分带性确定了含矿断裂;通过对燕山期侵入体的物化探特征研究,确定出25个含金岩体;叠加型异常是该区找矿的重点靶区。 Based on data of geology, geophysical-geochemical prospecting and remote sensing the geological background of metallization and ore-controlling factors for gold deposits in northeastern Shanxi are studied. The results indicat that the early Precambrian crystalline basement has close relation to metallization, and the iron-bearing formation of the Wutai Supergroup is an important source bed of gold deposits. Ore-bearing faults are determined by analysing of faults, primary anomalies and elementary zonation. 25 gold-bearing magmatic bodies are determined by analysing geophysical-geochemical characteristics of the Yanshanian intrusions. It is indicated that stacked anomalies are the main prospecting targets.
出处 《矿产勘查》 1995年第3期153-158,共6页 Mineral Exploration
关键词 物化探特征 含铁建造 叠加异常 geophysical-geochemical features iron-hearing formation stacked anomaly
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