J4

• 基础地质·矿床·盆地 • 上一篇    下一篇

新疆东昆仑锑富集特征及找矿前景分析

胡建卫1,郑启平2   

  1. 1.吉林大学 综合信息矿产预测研究所,长春 130026;2.新疆维吾尔自治区地质调查院,乌鲁木齐 830000
  • 收稿日期:2005-03-29 修回日期:1900-01-01 出版日期:2006-01-26 发布日期:2006-01-26
  • 通讯作者: 胡建卫

Study on Sb Enrichment and Exploration Potential for Sb Deposits in East Kunlun Mountain, Xinjiang

HU Jian-wei1, ZHENG Qi-ping2   

  1. 1.Institute of Mineral Resources Appraisal of Synthetic Information, Jilin University,Changchun 130026, China;2. Xinjiang Institute of Geological Survey, Urumqi 830000,China
  • Received:2005-03-29 Revised:1900-01-01 Online:2006-01-26 Published:2006-01-26
  • Contact: HU Jianwei

摘要: 新疆东昆仑存在一条长达700 km的锑异常带,在新疆该带锑元素富集程度最高、富集规模最大。西段的黄羊岭地区,已发现大面积锑矿化,其中的黄羊岭锑矿由4个长1 000~1 500 m、宽200~400 m的矿化带组成,含矿岩系为二叠系黄羊岭群碎屑岩,带内各类矿化脉体发育,锑矿化与石英脉关系密切,品位较富,呈现脉状矿化的特点,其资源远景在大型矿床规模以上。通过锑元素富集特征、控制因素、锑矿化特征及其与异常关系的研究,认为东昆仑地区具有寻找大型锑矿的地质-地球化学条件,该区资源潜力巨大,是新疆最有希望找大型锑矿的地区。

关键词: 新疆东昆仑, 锑元素富集带, 富锑块体, 黄羊岭锑矿

Abstract: There exists a Sb anomalous belt of 700 km long in the eastern Kunlun Mountains, which represents an area of most intensive and wide enrichment Sb in Xinjiang. A large scale of Sb mineralization has been discovered at Huangyangling in the western part of this huge Sb anomalous belt. The Huangyangling Sb deposit contains four mineralization zones with the length of 1000-1500 m and width of 200-400 m each. A series of mineralized veins occurred in the detrital rocks of the Permian Huangyangling Group. The Sb mineralization with highgrade ores is closely related to the quartz veins. The Huangyangling Sb deposit may be a potential giant one. On the basis of Sb enrichment coefficient, orecontrolling factors, and spatial relationship between Sb mineralization and anomaly, we suggest that the eastern Kunlun Mountains be of favorable geological, metallogenetic and geochemical conditions to host large or superlarge Sb deposits in Xinjiang.

Key words: East Kunlun Mountains of Xinjiang, Sb anomalous belt, blocks of Sb enrichment, Huangyangling Sb deposit

中图分类号: 

  • P618.66
[1] 丁清峰, 张本龙, 王冠, 金圣凯. 青海北巴颜喀拉成矿带基于专家证据权重法锑金矿资源潜力评价[J]. J4, 2011, 41(5): 1423-1431.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
[1] 张世广, 柳成志, 卢双舫, 张雁, 吴高平, 刘秋宏. 高分辨率层序地层学在河、湖、三角洲复合沉积体系的应用--以朝阳沟油田扶余油层开发区块为例[J]. J4, 2009, 39(3): 361 -368 .
[2] 李碧乐,沈鑫,陈广俊,杨延乾,李永胜. 青海东昆仑阿斯哈金矿Ⅰ号脉成矿流体地球化学特征和矿床成因[J]. 吉林大学学报(地球科学版), 2012, 42(6): 1676 -1687 .
[3] 杨晓平,李仰春,柳 震, 汪 岩,王洪杰. 黑龙江东部鸡西盆地构造层序划分与盆地动力学演化[J]. J4, 2005, 35(05): 616 -621 .
[4] 李发文, 冯平, 张超. 天津北三河地区垂向耦合产流模型及应用[J]. J4, 2011, 41(2): 459 -464 .
[5] 王立军,刘国才,黄继国,李跃迁,丛颖,沈照理,赵晓波. 接触氧化技术在公园景观水体功能恢复中的运用试验研究[J]. J4, 2006, 36(03): 458 -461 .
[6] 雷如雄,吴昌志,屈迅,顾连兴,陈刚,吾尔娜,孙洪涛,刘国宁. 中天山天湖东铁钼矿含矿片麻状花岗岩年代学、地球化学和锆石Hf同位素-对于中天山早古生代构造演化的启示[J]. 吉林大学学报(地球科学版), 2014, 44(5): 1540 -1552 .
[7] 初凤友,胡大千,姚杰. 中太平洋YJB海山富钴结核矿物组成与元素地球化学[J]. J4, 2007, 37(1): 8 -0014 .
[8] 周燕,郑培玺,王铁夫,张延洁. 招平断裂带上盘金矿床氢氧同位素地质特征[J]. J4, 2007, 37(4): 668 -0671 .
[9] 唐华风,王璞珺,姜传金,刘杰,张庆晨,冯有良. 松辽盆地火山岩相地震特征及其与控陷断裂的关系[J]. J4, 2007, 37(1): 73 -0078 .
[10] 范晓敏,李舟波. 裂缝性碳酸盐岩储层声波时差曲线的波动和增幅分析[J]. J4, 2007, 37(1): 168 -0173 .