摘要
浪木日镍多金属矿床是青海省有色地质矿产勘查局八队在东昆仑造山带东段发现的与基性—超基性侵入岩有关的岩浆熔离型铜镍硫化物矿床,在浪木日地区HS73号异常区发现2处规模不等的超基性岩体Σ1、Σ2,于Σ1超基性岩体中圈出镍多金属矿体1条(M1),并于HS71号综合异常区内发现Σ3含矿超基性岩体。浪木日地区与东昆仑造山带夏日哈木铜镍矿床具有相似的地质分布特征和地球化学特征,具有较好的矿化线索。综合分析得出,该区具有较大的找矿潜力。
The 8 th team of Qinghai nonferrous metals geological exploration bureau found Langmuri copper and nickel deposit in the east Kunlun orogenic belt and basic-ultrabasic intrusive rocks related to magmatic liquation copper and nickel sulfide ore deposit.In Langmuri HS73 anomaly area found two sizes of ultrabasic rock-Σ1,Σ2.In Σ1 ultrabasic rock,circled nickel polymetallic ore body1（ M1）.And in the HS71 comprehensive anomaly zone,it has found Σ3 ore ultrabasic rock mass.Langmuri area has great similar with Xiarihamu in geological distribution and geochemical characteristics.There are also good mineralization clues.In conclusion,the comprehensive analysis shows that the area has great potential for prospecting.
作者
施根红
熊生云
李永娜
王艳
张里斌
SHI Gen-hong;XIONG Sheng-yun;LI Yong-na;WANG Yan;ZHANG Li-bin(No.8 Team of Geology and Mineral Resources Bureau for Non-ferrous Metals of Qinghai Province,Xining 810012)
出处
《矿产勘查》
2018年第6期1205-1211,共7页
Mineral Exploration
基金
青海省地质勘查基金项目(编号:青国土资矿[2017]151)
中国地质调查局项目(编号:12120114081401)联合资助
关键词
东昆仑造山带
浪木日地区
镍多金属矿
超基性岩体
成矿潜力
East-Kunlun orogenic belt
Langmuri area
nickel polymetallic deposit
ultrabasic rock mass
metallogenic potential
