img

QQ群聊

img

官方微信

高级检索

黄金科学技术 ›› 2016, Vol. 24 ›› Issue (6): 32-38.doi: 10.11872/j.issn.1005-2518.2016.06.032

• 矿产勘查与资源评价 • 上一篇    下一篇

内蒙古桦树沟金矿综合找矿效果及意义

吴家富,王翔,黄俊   

  1. 安徽省地质调查院,安徽  合肥   230001
  • 收稿日期:2016-02-23 修回日期:2016-09-14 出版日期:2016-12-28 发布日期:2017-01-22
  • 作者简介:吴家富(1968-),男,安徽巢湖人,高级工程师,从事区域矿产地质调查工作。ahwjf103@sina.com
  • 基金资助:

    内蒙古地质勘查基金项目“内蒙古乌兰察布市察哈尔右翼前旗等四幅1∶5万区域矿产地质调查”(编号:[2008]矿调2-22)资助

Comprehensive Prospecting Effect and Significance of Huashugou Gold Deposit in Inner Mongolia

WU Jiafu,WANG Xiang,HUANG Jun   

  1. Anhui Institute of Geological Survey,Hefei    230001,Anhui,China
  • Received:2016-02-23 Revised:2016-09-14 Online:2016-12-28 Published:2017-01-22

摘要:

在1/5万察哈尔右翼前旗等四幅区域矿产地质调查的基础上,通过化探系统采集样品、地质填图和综合找矿方法发现了桦树沟金矿,并对金矿成矿提出了新的认识。野外地质研究发现,桦树沟矿区NE、近EW向断裂控制着异常展布及地表构造蚀变带和铁锰矿化体的延伸,围岩及矿化蚀变主要有硅化、钾化、绢云母化及沿裂隙充填的铁锰矿化和褐铁矿化。运用综合找矿方法筛选找矿靶区,将桦树沟异常面积从28.8 km2缩小到3.6 km2,有助于更好地找寻金矿床。采用水系沉积物和土壤测量方法对矿区异常元素进行了测试,并根据富集系数讨论富集成矿问题,结果显示:与成矿关系密切的桦树沟岩体强富集元素有Ag、Pb、Zn、As、Sb、W、Bi和Mo等,其围岩集宁岩群富集—强富集元素有Ag、Pb、Au、Cu、As、Sb、W和Mo等,表明岩浆活动为成矿提供了含矿热液,而热液又与围岩发生交代,导致金银等多金属在成矿有利部位富集成矿。结合1/1万地质填图、1/1万土壤测量等方法进一步开展异常检查评价,发现多个样品含量已达矿石边界品位,异常浓集中心及分带明显,经探槽工程揭露并圈定出2条金矿体,其分布特征、物质组成和控矿因素已基本查明,表明该区具有良好的找矿前景。

关键词: 综合找矿, 地球化学, 桦树沟金矿, 内蒙古

Abstract:

 Huashugou gold mine was found,and the new understanding of gold mineralization was put forward basis on the geological survey in four 1/50000 regional map of Chahar right Qianqi,etc,by using the geochemical samples exploration,geological mapping and the comprehensive prospecting methods.Field geological study found that NE and nearly EW trend faults control the distribution of the abnormal faults and the outspread of the surface structure alteration belt and iron manganese ore body in the mining area.The surrounding rock and mineralization alteration are mainly silicide,potassium,sericitization and along the fissure filling iron manganese ore and limonite.Selecting the prospecting target area by comprehensive prospecting method,Huashugou anomaly area were reduced from 28.8 km2 to 3.6 km2,help to better looking for gold deposit.By using stream sediment and soil measurement method,anomaly elements were tested,and according to the enrichment coefficient,the results showed that Ag,Pb,Zn,As,Sb,W,Bi,Mo,etc.,has strong enrichment in Huashugou groove rock,and closely associated with mineralization,its surrounding rock,the Jining Group are enrich and strong enrich in Ag,Pb,Au,Cu,As,Sb,W,Mo,etc.,show that magma activity provides a ore-bearing hydrothermal mineralization,and hydrothermal metasomatic with surrounding rock,causing much metals such as gold and silver enrichment in the favourable area.Combining 1/10000 geological mapping methods and soil measuring,further anomaly examination and evaluation was conducted,found multiple ore sample content with cutoff grade,obvious abnormal thick concentrated heart and zoning.The implementation of exploratory trench engineering expose and mark out 2 gold orebodies,the distribution feature,composition and ore-controlling factors have been identified,indicating that the area has good ore prospects.

Key words: comprehensive prospecting, geochemistry, Huashugou gold deposit, Inner Mongolia

中图分类号: 

  • P618.51

[1] 黄俊,薛全君,吴家富,等.内蒙古桦树沟金矿区成矿地质特征及找矿方向[J].黄金科学技术,2013,21(4):15-19.
[2] 任天祥,伍宗华,羌荣生.区域化探异常筛选与查证的方法技术[M].北京:地质出版社,1998.
[3] 中华人民共和国地质矿产行业标准.地球化学普查规范(比例尺1∶50000):DZ/T0011-91[S].北京:中国标准出版社,1996.
[4] 中华人民共和国地质矿产行业标准.地球化学普查规范:DZ/T0145-94[S].北京:中国标准出版社,1995.
[5] 内蒙古自治区地质矿产局.内蒙古自治区区域地质志[M].北京:地质出版社,1991.
[6] 吴家富,黄俊,王翔,等.内蒙古乌兰察布市察哈尔右翼前旗等四幅1∶5万区域矿产地质调查成果报告[R].集宁:内蒙古自治区有色地质勘查局609队,2012.
[7] 刘桂阁,李艳秋,常春郊,等.区域化探数据处理的综合异常法研究[J].黄金科学技术,2012,20(4):67-69.
[8] 龚美菱.评价金化探异常的新方法[J].有色金属矿产与勘查,1995,4(2):100-106.
[9] 罗先熔,文美兰,欧阳菲,等.勘查地球化学[M].北京:冶金工业出版社,2007.
[10] 申伍军,王学求.内蒙古大型银矿集区地球化学预测[J]. 地球学报,2010,31(3):449-455.
[11] 黄俊,吴家富,鲁如魁,等.内蒙古兵图金矿成因探讨及找矿方向[J].黄金科学技术,2010,18(4):1-5.
[12] 夏冬,牛树银,徐国,等.内蒙古哈达门沟金矿控矿机制[J].黄金科学技术,2011,19(2):13-17.

[1] 陈懋弘, 谢贤洋, 马克忠. 贵州泥堡卡林型金矿断控型矿体的地层和岩性条件研究[J]. 黄金科学技术, 2018, 26(2): 131-142.
[2] 曲晖, 王佰义, 王建民, 李成禄, 徐国战, 王卓. 土壤地球化学测量在永新金矿勘查中的应用及找矿效果研究[J]. 黄金科学技术, 2018, 26(2): 143-152.
[3] 张健,杨兴科*,晁会霞,何虎军,韩珂,杨龙伟,李斌. 南秦岭石泉—汉阴北部金矿带矿化蚀变特征[J]. 黄金科学技术, 2017, 25(6): 21-30.
[4] 郑慕婷,张术根,贺忠春. 湖南康家湾金银多金属矿床金银赋存状态及其与成矿演化的关系[J]. 黄金科学技术, 2017, 25(6): 31-42.
[5] 梁永科,王德恭,赵杰. 湖南玉横塘金矿区地质特征及找矿前景分析[J]. 黄金科学技术, 2017, 25(6): 43-51.
[6] 高帅,曾庆栋,于昌明,邢宝山,荆林海,叶杰,范宏瑞,杨奎锋. 遥感及综合物探方法用于山东招远南部隐伏成矿侵入体的空间定位[J]. 黄金科学技术, 2017, 25(5): 1-10.
[7] 韩珂,杨兴科*,张健,胡国朝. 陕南汉阴黄龙金矿脆—韧性剪切带特征及其对成矿的控制作用[J]. 黄金科学技术, 2017, 25(5): 18-29.
[8] 王晓青,杨兴科,芮会超. 内蒙古岱王山金矿黄铁矿形态标型及其变化规律与找矿意义[J]. 黄金科学技术, 2017, 25(5): 39-46.
[9] 陈彩华,孙斌,陈冀,陈力子 . 西秦岭中寨—十里铺地区水系沉积物测量找矿效果[J]. 黄金科学技术, 2017, 25(4): 1-9.
[10] 张磊,佟宇,杨振东,白云龙,刘幸,赵永涛. 辽宁苇子沟地区金铜多金属矿成矿机制及找矿方向[J]. 黄金科学技术, 2017, 25(4): 10-17.
[11] 宋英昕,宋明春,丁正江,魏绪峰,徐韶辉,李杰,谭现峰,李世勇,张照录, 焦秀美,胡弘,曹佳. 胶东金矿集区深部找矿重要进展及成矿特征[J]. 黄金科学技术, 2017, 25(3): 4-18.
[12] 宋国政,闫春明,曹佳,郭志峰,鲍中义,刘国栋,李山,范家盟,刘彩杰. 胶东焦家成矿带超千米深部金矿勘查突破及意义——以纱岭矿区为例[J]. 黄金科学技术, 2017, 25(3): 19-27.
[13] 徐忠华,王福江,周明岭,白宜娜,赵成乐,胡秉谦. 胶东磨山金矿床主要金属矿物的矿物学特征及矿床成因研究[J]. 黄金科学技术, 2017, 25(3): 28-37.
[14] 刘国栋,温桂军,刘彩杰,鲍中义*,孙忠全,范家盟,李山,闫春明,郭志峰. 招平断裂北段水旺庄深部超大型金矿床的发现、特征和找矿方向[J]. 黄金科学技术, 2017, 25(3): 38-45.
[15] 万鹏,丁正江,胡弘,吴凤萍,程蓉蓉,邹键 . 胶东邓格庄金矿床深部成矿特征及找矿方法组合[J]. 黄金科学技术, 2017, 25(3): 46-53.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!