若羌塔木切伟晶岩型锂铍稀有多金属矿床成因分析及找矿标志  

Gentic analysis and Prospecting Criteria of Tamuchi Pegmatitic Type Lithium Beryllium Rare Poiymetallic Deposit in Ruoqiang County,XinJiang Province

作　　者：陈德本 陈晋 刘豹 陈煌 陈建中[1] 代鸿章 Chen Deben;Chen Jin;Liu Bao;Chen Huang;Chen Jianzhong;Dai Hongzhang(The Third Geological Branch,Xinjiang Geological and Mineral Bureau,Kuerle,Xinjiang 841000,China;MNR Key Laboratory of Metallogeny and Mineral Assessment,Institute of Mineral Resource CAGS,Beijing 100037,China)

机构地区：[1]新疆维吾尔自治区地质矿产勘查开发局第三地质大队,新疆库尔勒841000 [2]自然资源部成矿作用与资源评价重点实验室,中国地质科学院矿产资源研究所,北京1000372

出　　处：《新疆地质》2024年第2期259-263,共5页Xinjiang Geology

基　　金：新疆维吾尔自治区地质局地质勘查项目(XGMB202240、XGMB202207);中国地质调查局地质调查项目(KD-2019-XZ-141、KD-2020-XZ-117、KD-2021-XZ-076、KD-2023-XZ-111)联合资助。

摘　　要：花岗伟晶岩型锂矿是锂资源的重要类型之一,也是当前国际矿床学研究的热点。对阿尔金花岗伟晶岩型锂铍稀有金属成矿带典型矿床-塔木切花岗伟晶岩型锂铍稀有多金属矿成因进行分析,总结找矿标志,为该区域寻找同类型矿床提供参考。The granite-pegmatite-type lithium deposit is one of the most important types of lithium resources,and it is also a hot spot in the international ore deposit research.The granite-pegmatite-type lithium beryllium rare metal metallogenic belt of the west Altun Member is a major breakthrough of lithium beryllium rare metal deposits made in Xinjiang in recent years.This paper attempts to analyze the genesis of the typical deposit in this metallogenic belt,the Tamucean granite pegmatite-type lithium beryllium rare polymetallic deposit,and summarize it The prospecting indicator can provide reference for regional prospecting of similar type of deposits.

关 键 词：塔木切 花岗伟晶岩型锂铍矿 成因分析 找矿标志 

分 类 号：P618.6[天文地球—矿床学]