| 赵鹏彬,张继军,高云鹏,周栋,李毅,张童.内蒙风化梁北金矿区地质特征及找矿潜力分析[J].矿产勘查,2019,(1):33-40 |
| 内蒙风化梁北金矿区地质特征及找矿潜力分析 |
| Geological characteristics and prospecting potential analysis of Fenghualiang gold mine area in Inner Mongolia |
| 投稿时间：2018-07-03 |
| DOI： |
| 中文关键词: 金矿 地质特征 构造蚀变岩型 找矿潜力 内蒙北山 |
| 英文关键词: geological characteristics ,gold deposits, structural altered rock type ,prospecting potential, Beishan, inner Mongolia |
| 基金项目:内蒙古自治区地质勘查基金项目(编号:04-2-KD05,06-2-KC24和NMKD2014-09)资助。 |
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| 中文摘要: |
| 风化梁北金矿区位于北西向风化梁断裂带以南,石炭纪英云闪长岩与志留纪公婆泉组接触带上,北西向多期活动断裂为主要控矿容矿构造。文章通过对矿区的地质特征、地球化学特征、矿(化)体特征及围岩蚀变、矿床成因的分析,结合地球物理测深资料,认为该金矿为构造蚀变岩型,深部显示良好的找矿潜力。 |
| 英文摘要: |
| The Fenghualiang Au mining area is located to the south of Fenghualiang fault zone. the contact zone Located on the contact belt between carboniferous tonalite and SILURIAN gongpoquan formation. the multi-stage active fault is the main ore-controlling and ore-hosting structure. By expounded and analyzed the geological characteristics, geochemical characteristics, ore ( mineralized ) body characteristics, wall rock alteration and genesis of the deposit in the mining area, combined with geophysical data, it is believed that the gold deposit is a structural altered rock type with good prospecting potential in the deep part. further work is expected to make a breakthrough in prospecting in the deep part. |
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