首页|铁矿矿床地质特征及找矿标志研究

铁矿矿床地质特征及找矿标志研究

Research on Geological Characteristics and Ore Exploration Cri-teria of Iron Ore Deposits

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本研究聚焦于特定区域的铁矿矿床,通过对矿床地质特征和找矿标志的深入研究,揭示了铁矿矿床的地质结构、成矿条件及成因机制.研究发现,该区域铁矿体受特定地层的严格控制,与围岩差异显著,为地球物理和地球化学勘查提供了明确的找矿标志.此外,褶皱构造与断裂系统的活动为铁矿成矿提供了有利的空间条件.本研究不仅为未来铁矿勘探与开发提供了科学依据,也为铁矿矿床地质学的发展及我国铁矿资源勘查能力的提升贡献了新的认识与思路.后续找矿工作应侧重于对复向斜北翼磁异常区的深入探索,以期为我国铁矿资源的可持续利用奠定坚实基础.
This study focuses on iron ore deposits in specific regions,and through in-depth research on the geological charac-teristics and prospecting indicators of the deposits,reveals the geological structure,mineralization conditions,and genetic mechanisms of iron ore deposits.Research has found that the iron ore bodies in this area are strictly controlled by specific geo-logical strata and differ significantly from the surrounding rocks,providing clear prospecting indicators for geophysical and geo-chemical exploration.In addition,the activity of fold structures and fault systems provides favorable spatial conditions for iron ore mineralization.This study not only provides scientific basis for future iron ore exploration and development,but also con-tributes new understanding and ideas for the development of iron ore deposit geology and the improvement of China's iron ore resource exploration capabilities.The follow-up exploration work should focus on in-depth exploration of the magnetic anoma-ly area on the northern wing of the synclinal,in order to lay a solid foundation for the sustainable utilization of iron ore resourc-es in China.

iron ore depositgeological featuresmagnetiteore finding signs

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山东金莱矿业有限公司,山东莱州 261413

铁矿矿床 地质特征 磁铁矿 找矿标志

2024

新疆钢铁
新疆维吾尔自治区金属学会

新疆钢铁

影响因子:0.081
ISSN:1672-4224
年,卷(期):2024.(3)