团结沟金矿外围十三公里区隐伏矿体预测

• 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.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.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/Abstract

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

吴国学，李守义，吕志刚，王永祥，汪振涌，崔敏. 团结沟金矿外围十三公里区隐伏矿体预测[J]. J4, 2006, 36(05): 781-786.

WU Guo-xue, LI Shou-yi, LV Zhi-gang,WANG Yong-xiang, WANG Zhen-yong, CUI Min. The Prognosis of the Concealed Orebodies in the Shisangongli Area Nearby the Tuanjiegou Gold Deposit[J]. J4, 2006, 36(05): 781-786.

参考文献

Metrics

Viewed

Full text

Abstract

Cited

Shared

Discussed

本文评价

推荐阅读 10

[1]	尤敏鑫，刘建民. 同位素地球化学在峨眉山大火成岩省研究中的应用现状与进展[J]. 吉林大学学报(地球科学版), 2014, 44(4): 1231 -1243 .
[2]	杨春梅, 李洪奇,陆大卫,张方礼,高原,邵英超. 不同驱替方式下岩石电阻率与饱和度的关系[J]. J4, 2005, 35(05): 667 -671 .
[3]	祝洪臣，张炯飞，权恒. 大兴安岭中生代两期成岩成矿作用的元素、同位素特征及其形成环境[J]. J4, 2005, 35(04): 436 -0442 .
[4]	朱建伟, 赵刚, 刘博, 郭巍, 成俊. 油页岩测井识别技术及应用[J]. J4, 2012, 42(2): 289 -295 .
[5]	陈力，梁海安，张文娟，荣帆. 模糊数学方法在城市工程地质环境区划中的应用--以抚顺市城区为例[J]. J4, 2008, 38(5): 837 -0840 .
[6]	高桂梅,苏克,王文颖,甘树才,刘招君. 吉林省桦甸油页岩中稀土元素和微量元素的研究[J]. J4, 2006, 36(6): 974 -0979 .
[7]	吴孔运，蒋忠诚，叶晔. 不同植物群落对灰岩试块溶蚀速率的影响[J]. J4, 2007, 37(5): 967 -0971 .
[8]	周彦章，迟宝明，刘中培. 山东夏甸金矿床充水机理构造控制模式[J]. J4, 2008, 38(2): 255 -0260 .
[9]	张渊，刘连登，孙景贵，陈国华，张洪喜，闫复传,杨开春. 胶东西北部黄埠岭金矿床两期次叠加成矿[J]. J4, 2008, 38(1): 21 -0026 .
[10]	鲁程鹏, 束龙仓, 苑利波, 张蓉蓉, 黄币娟, 王彬彬. 基于示踪试验求解岩溶含水层水文地质参数[J]. J4, 2009, 39(4): 717 -721 .