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现代地质 ›› 2024, Vol. 38 ›› Issue (01): 87-97.DOI: 10.19657/j.geoscience.1000-8527.2024.005

• 中国东部富铁矿成矿机制与找矿预测 • 上一篇    下一篇

基于地球物理技术圈定沉积变质型富铁矿体: 辽宁鞍山齐大山铁矿例析

蒙嘉琪1(), 王志猛2, 贾三石1,3,4, 付建飞1(), 张岩松1   

  1. 1.东北大学资源与土木工程学院,辽宁 沈阳 110000
    2.鞍钢集团矿业弓长岭有限公司井采分公司,辽宁 辽阳 111000
    3.东北大学秦皇岛分校资源与材料学院,河北 秦皇岛 066004
    4.海洋油气勘探国家工程研究中心,北京 100028
  • 收稿日期:2023-07-31 修回日期:2024-01-10 出版日期:2024-02-10 发布日期:2024-03-20
  • 通讯作者: 付建飞,男,博士,副教授,1973年出生,地质学专业,主要从事资源环境探测与评价研究。Email:fujianfei@mail.neu.edu.cn
  • 作者简介:蒙嘉琪,男,硕士研究生,1999年出生,地质资源与地质工程专业,主要从事资源探测研究。Email:2201081@stu.neu.edu.cn
  • 基金资助:
    国家重点研发计划项目(2022YFC2903701)

Delineation of Sedimentary Metamorphic Rich Iron Ore Bodies Based on Geophysical Techniques: Case Analysis of Qidashan Iron Ore in Anshan, Liaoning

MENG Jiaqi1(), WANG Zhimeng2, JIA Sanshi1,3,4, FU Jianfei1(), ZHANG Yansong1   

  1. 1. School of Resources and Civil Engineering, Northeastern University, Shenyang, Liaoning 110000, China
    2. Angang Group Mining Gongchangling Co.LTD. Well Mining Branch, Liaoyang, Liaoning 111000, China
    3. College of Resources and Materials, Qinhuangdao Campus, Northeastern University, Qinhuangdao, Hebei 066004, China
    4. National Engineering Research Center for Offshore Oil and Gas Exploration, Beijing 100028, China
  • Received:2023-07-31 Revised:2024-01-10 Online:2024-02-10 Published:2024-03-20

摘要:

辽宁鞍山—本溪地区是中国北方最重要的铁矿资源基地之一,区内分布有数量不等的富铁矿体,长期以来对富铁矿成矿理论研究成果丰硕,但针对富铁矿找矿技术方面的研究则相对缺乏。本文以辽宁鞍山齐大山铁矿为研究对象,基于贫铁矿体和富铁矿体的物性参数差异,优选地面高精度磁法和高密度电阻率法,开展齐大山铁矿内富铁矿体的综合地球物理探测研究工作。研究结果显示,地面高精度磁法可以通过16000 nT以上的高磁场强度特征圈出贫铁矿磁异常场内的富铁矿体,而高密度电阻率法则可以精细刻画高磁异常范围内的富铁矿体形态特征和规模;磁铁矿富矿电阻率小于2200 Ω·m,以此为约束条件构建地面磁法的正反演模型,可实现对贫铁矿层中富铁矿体的准确识别定位;齐大山铁矿NNW走向断层与NEE横向断层交汇处更易产出厚大富铁矿体。

关键词: 鞍本地区, 富铁矿, 高精度磁法, 高密度电阻率法, 识别定位

Abstract:

Anshan-Benxi Area of Liaoning Province is one of the most important iron resource bases in Northern China. There are various iron-rich orebodies distributed in this area. The studies on the iron-rich ore metallogeny are fruitful for the past decades but the prospecting technology for iron-rich ores is relatively lacking. Based on the discrepancy of physical parameters between the iron-poor and -rich orebodies, we selected surface high-precision magnetic and high-density resistivity methods to perform the comprehensive geophysical exploration of the iron-rich orebodies in the Qidashan iron mine area in Anshan, Liaoning Province. The study results show that the high-precision magnetic method is able to delineate the spatial distribution range of the magnetic anomalies caused by the enriched iron bodies in the magnetic anomaly field with a poor iron grade through limiting the magnetic field intensity at >16,000 nT. The high-density resistivity method can accurately characterize the shape and scale of iron-rich bodies in the high magnetic anomaly field by limiting the resistivity at <2200 Ω·m. This can be considered as a constraint threshold to build a forward and inverse models for the ground magnetic method as to identify and locate the iron-rich bodies in iron-poor ore layers. We also found that the intersection area of the NNW strike and NEE lateral fault in Qidashan iron mine area has a higher potential to form thick and enriched iron orebodies.

Key words: Anshan-Benxi Area, iron-rich mine, high-precision magnetic method, high-density resistivity method, ore identification and location

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