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• 基础地质·矿床·盆地 • 上一篇    下一篇

团结沟金矿外围十三公里区隐伏矿体预测

吴国学1,李守义1,吕志刚1,王永祥1,汪振涌2,崔敏1   

  1. 1.吉林大学 地球科学学院, 长春 130061;2.黑龙江乌拉嘎金矿,黑龙江 伊春 153221
  • 收稿日期:2006-05-17 修回日期:1900-01-01 出版日期:2006-09-26 发布日期:2006-09-26
  • 通讯作者: 吴国学

The Prognosis of the Concealed Orebodies in the Shisangongli Area Nearby the Tuanjiegou Gold Deposit

WU Guo-xue1, LI Shou-yi1, LV Zhi-gang1,WANG Yong-xiang1, WANG Zhen-yong2, CUI Min1   

  1. 1.College of Earth Sciences,Jilin University, Changchun 130061,China;2.Heilongjiang Wulaga Gold Deposit,Yichun,Heilongjiang 153221,China
  • Received:2006-05-17 Revised:1900-01-01 Online:2006-09-26 Published:2006-09-26
  • Contact: WU Guo-xue

摘要: 通过团结沟金矿成矿背景与矿区地质的研究,建立了矿床综合找矿模型。对团结沟金矿外围十三公里区地质信息、高精度磁测信息、γ能谱信息及土壤地球化学信息的分析,确定了该区综合找矿信息特征,并进行隐伏金矿体预测。通过对比团结沟金矿床综合找矿模型,对异常区进行优选,并对优选出的靶区实施了工程查证,探槽及浅井双双见矿,共获得黄金资源量1.5 t。隐伏金矿体预测效果显著,矿区外围有巨大的增储前景。

关键词: 团结沟金矿, 隐伏矿体, 综合找矿模型, 矿体预测

Abstract: Based on the research on the metallogenic setting and on the mine geology of the Tuanjiegou gold deposit, a synthesis exploring model for the deposit has been set up. The characters of synthe-tical exploring information about the area have been summarized according the geological information, high precision magnetic measurement, γ-ray spectrum testing and geochemical information of soil carried out and the concealed gold orebodies have been forecasted. By compared to the synthetical exploring model of the Tuanjiegou gold deposit, the most favorable targets for the concealed orebodies were selected and tested. Gold ores were found in both exploratory trenches and shafts, and gold ores with 1.5t gold have been proven. It proves that the present forecasting efforts are successful and there is great potential also for gold searching around the Tuanjiegou gold deposit.

Key words: Tuanjiegou gold deposit, concealed ore body, synthesis exploring model, orebodies forecasting

中图分类号: 

  • P618.51
[1] 曹建劲, 李映葵, 刘昶, 袁雪玲. 贵州关岭丙坝铜矿床地气微粒特征[J]. 吉林大学学报(地球科学版), 2017, 47(1): 95-105.
[2] 张作伦,曾庆栋,叶杰,贾长顺,李文涛. 草原覆盖区隐伏金属矿体定位预测--以大兴安岭中南段某铅锌矿点为例[J]. J4, 2007, 37(1): 38-0040.
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