摘要
那拉提成矿带位于西天山偏西方向的区段上,属于那拉提山主脊线周围区域。为阿特巴什、伊内里切克、那拉提巨型构造带的一部分,该区与中亚成矿域非常接近,是其向东延续到我国西天山区域的范围,其成矿背景具有相似之处。乔霍特铜矿带以及箐布拉克铜镍铂矿带二者之间的区域上是该矿的分布所在,属于那拉提-红柳河成矿带。金铜矿化在此具有非常有利的赋存地层。文中笔者对那拉提成矿带铜金矿地质特征进行分析的基础上,探讨其找矿前景。为那拉提地区更加深入的地质研究工作提供参考。
Nalati mineralization belt is located in the Western Tianshan Mountains west direction section, which belongs to the Nalati mountain area around the main ridge line. It is a part of the mega structural belt of atbaash, irinchke and nerarti, which is very close to the Central Asian metallogenic domain, which extends eastward to the West Tianshan area in China, and its metallogenic background is similar. The area between the two Joholt copper ore belts and the qingBraque copper nickel platinum ore belt is the distribution of the ore. It belongs to the natural river of red river. Au Cu mineralization has a very favorable occurrence stratum. Based on the geological characteristics of gold ore belt znalati copper on the analysis of its prospecting potential. To provide reference for further geological research work in Nalati area.
作者
杨超
YANG Chao(Second regional geological survey of Xinjiang geological and Mining Bureau,Changji 831100,China)
出处
《世界有色金属》
2018年第5期130-130,132,共2页
World Nonferrous Metals
基金
新疆奇台县乌伦布拉克 -乌力牙斯克铜
镍矿普查项目资助
关键词
那拉提成矿带
地质特征
找矿前景
Nalati mineralization zone
geological characteristics
prospecting potential
