欢迎访问《金属矿山》杂志官方网站,今天是 分享到:
×

扫码分享

金属矿山 ›› 2025, Vol. 54 ›› Issue (7): 233-242.

• 地质与测量 • 上一篇    下一篇

栾川县石窑沟钼钨矿区地物化综合找矿模型

吕宪河  刘俊涛  胡红雷  宁  勇  王海勇  霍清华   

  1. 河南省地质研究院,河南 郑州 450001
  • 出版日期:2025-07-15 发布日期:2025-08-14
  • 通讯作者: 刘俊涛(1968—),男,高级工程师。
  • 作者简介:吕宪河(1973—),男,高级工程师
  • 基金资助:
    河南省 2008 年度两权价款地质勘查项目(编号:豫国土资发〔2009〕93 号)

Comprehensive Geophysical and Geochemical Prospecting Model of the Shiyaogou Molybdenum-Tungsten Deposit in Luanchuan County 

LÜ Xianhe  LIU Juntao  HU Honglei  NING Yong  WANG Haiyong  HUO Qinghua    

  1. Henan Academy of Geology,Zhengzhou 450001,China
  • Online:2025-07-15 Published:2025-08-14

摘要: 栾川县石窑沟钼钨矿区地处华北陆块南缘与北秦岭造山带的结合部位,该区域经历了多期次构造运 动,区域上广泛出露燕山期花岗岩体,具有良好的成矿地质条件。 针对 1 ∶5 万化探综合异常,结合矿区地质特征和物 化探特征,系统分析了地质、地球化学和地球物理信息之间的内在联系,构建了地物化综合信息找矿模型。 该模型融 合了地质背景分析、地球化学异常追踪与地球物理深部探测,实现了不同方法优势互补,在该区域取得了理想的找矿 成效。 研究表明:① 地质测量初步查明了矿区的成矿地质背景,钼矿化多产于岩体与四岔口岩组外接触带及内接触 带附近,钼钨矿与早白垩世侵入岩关系密切;② 通过 1 ∶1 万土壤剖面测量,圈定了铜钨钼综合异常,土壤异常与 1 ∶5 万水系异常浓集中心基本吻合,表明该区具有 Mo、W、Bi 等成矿元素的局部富集特征;③ 激电中梯测量和激电测深结 果显示,矿区存在明显的高阻高极化异常,与矿体产出部位基本吻合;④ 综合运用地质、地球化学和地球物理方法,构 建了石窑沟钼钨矿区的综合找矿模型,为该区成矿预测提供了科学依据;⑤ 依据综合信息找矿模型,在石窑沟钼钨矿 区共圈出钼矿体 1 条,钼矿化体 10 条,钨矿化体 4 条,钼钨矿化体 1 条,其中 12 # 钼矿体分为东西两段,控制长度 135 m,厚 0. 94~ 2. 16 m,品位 0. 112% ~ 0. 149%,取得了显著的找矿成果。 

关键词: 钼钨矿  化探综合异常  找矿标志  找矿模型 

Abstract: The Shiyaogou molybdenum-tungsten deposit in Luanchuan County is located at the junction of the southern margin of the North China Block and the North Qinling Orogenic Belt. This area has experienced multiple phases of tectonic movements,and Yanshanian granite bodies are widely exposed in the region,which provides favorable geological conditions for mineralization. According to the 1 ∶50 000 comprehensive geochemical anomalies,combined with the geological characteristics, geochemical and geophysical characteristics of the deposit,the internal relationships among geological,geocheical and geophysical information were systematically analyzed,and the comprehensive geological,geochemical and geophysical prospecting model was established. This model integrates geological background analysis,geochemical anomaly tracing and geophysical deep detection,realizing the complementary advantages of different methods,and has achieved ideal prospecting results in the application practice of this area. The research shows that:① Geological survey preliminarily identified the metallogenic geological background of the deposit. Molybdenum mineralization mostly occurs in the outer contact zone and near the inner contact zone between the rock mass and the Sichakou Formation,and molybdenum-tungsten ore is closely related to the Early Cretaceous intrusive rocks. ② Through the 1 ∶10 000 soil profile survey,the comprehensive anomalies of copper,tungsten and molybdenum were delineated. The soil anomalies basically coincide with the concentration centers of the 1 ∶50 000 stream sediment anomalies,indicating that this area has the local enrichment characteristics of metallogenic elements such as Mo,W and Bi. ③ The results of IP intermediate gradient survey and IP sounding show that there are obvious high-resistance and high-polarization anomalies in this area,which basically coincide with the occurrence positions of the orebodies. ④ By comprehensively utilizing geological,geochemical and geophysical methods,an comprehensive prospecting model for the Shiyaogou molybdenum-tungsten deposit was established,providing a scientific basis for the metallogenic prediction in this area. ⑤ According to the Comprehensive information prospecting model,a total of 1 molybdenum orebody,10 molybdenum mineralized bodies,4 tungsten mineralized bodies and 1 molybdenum-tungsten mineralized body were identified in the Shiyaogou molybdenum-tungsten deposit. Among them,the 12 # molybdenum orebody is divided into two sections,east and west,with a controlled length of 135 m,a thickness of 0. 94~ 2. 16 m,and a grade of 0. 112% ~ 0. 149%,achieving remarkable exploration results. 

Key words: molybdenum-tungsten ore,comprehensive geochemical anomaly,prospecting indicator,prospecting model 

中图分类号: