新疆哈密市乌岭北锰矿床特征及成因分析  

Characteristics and genesis of Wuling North Manganese Deposit in Hami City, Xinjiang

作　　者：李艳[1] LI Yan(First Regional Geological Survey Brigade of Xinjiang Uygur Autonomous Region Geological and Mineral Exploration and Development Bureau,Urumqi 830011,China)

机构地区：[1]新疆维吾尔自治区地质矿产勘查开发局第一区域地质调查大队

出　　处：《世界有色金属》2019年第6期264-265,共2页World Nonferrous Metals

摘　　要：乌岭北锰矿是近年来在新疆哈密地区新发现的一个锰矿床,该矿位于新疆东部雅满苏北山一带。锰矿体主要产出于上石炭统梧桐窝子组火山碎屑岩夹透镜状硅质岩组合中。本文对该矿成矿地质特征及矿体特征进行分析,初步认为矿床成因类型为海相沉积锰矿床,总结了矿床成因及相关找矿标志。Wuling North Manganese Deposit is a newly discovered manganese deposit in Hami area of Xinjiang. It is located in the Beishan area of Yamansu in eastern Xinjiang. Manganese ore bodies occur mainly in the upper Carboniferous Wutongwozi Formation volcaniclastic rocks with lenticular siliceous rock assemblages. In this paper, the metallogenic geological characteristics and ore body characteristics of the deposit are analyzed. It is preliminarily considered that the genetic type of the deposit is marine sedimentary manganese deposit. The genesis of the deposit and related prospecting criteria are summarized.

关 键 词：乌岭北锰矿 矿床特征 成因分析 

分 类 号：P619.28[天文地球—矿床学]