吉林省舒兰市长安堡斑岩钼矿床成矿作用及成矿地球动力背景  

Metallogenesis and geodynamic setting of Chang’anpu porphyry Molybdenum deposit in Shulan City,Jilin Province

作　　者：张剑[1,2] ZHANG Jian(College of Earth Sciences,Jilin University,Changchun 130061,China;Jilin Nonferrous Metal Geological Exploration Bureau,Team 607,Jilin 132105,China)

机构地区：[1]吉林大学地球科学学院,吉林长春130061 [2]吉林省有色金属地质勘查局六〇七队,吉林吉林132001

出　　处：《世界有色金属》2021年第23期80-82,共3页World Nonferrous Metals

摘　　要：吉林省舒兰市长安堡大型斑岩钼矿床位于小兴安岭-张广才岭成矿带内,为近几年在东北地区发现的又一个大型斑岩钼矿床,本文较详细地介绍了长安堡斑岩钼矿床的地质特征,对成矿地质作用及成矿地球动力背景进行深入讨论,对今后在东北地区寻找中生代斑岩型矿床提供借鉴和参考。The Chang’anpu large porphyry molybdenum deposit in Shulan City,Jilin Province is located in the Lesser Khingan Mountains-Zhangguangcai Mountains metallogenic belt,which is another large porphyry molybdenum deposit discovered in northeast China in recent years.This paper introduces the geological characteristics of Chang’anpu large porphyry molybdenum deposit in detail,and discusses the genesis of the deposit and the source of ore-forming materials in depth.It provides reference for future exploration of Mesozoic porphyry deposits in northeast China.

关 键 词：斑岩钼矿床 矿床地质特征 成矿作用 成矿地球动力背景 

分 类 号：P597.3[天文地球—地球化学]