文章摘要
李金超.青海省东昆仑成矿带主要金矿床特征与及关键控矿因素分析[J].地质与勘探,2015,51(6):1079-1088
青海省东昆仑成矿带主要金矿床特征与及关键控矿因素分析
Characteristics of gold deposits and ore-control factors in the East Kunlun mineralization belt, Qinghai Province
投稿时间:2015-10-03  修订日期:2015-11-22
DOI:
中文关键词: 金矿 控矿因素 成矿潜力 东昆仑 青海
英文关键词: East Kunlun region, gold deposit, ore-controlling factor, metallogenetic potentiality
基金项目:国土资源大调查项目(编号:1212010918044、12120113029000、12120115022101)联合资助。
作者单位E-mail
李金超 西安地质矿产研究所国土资源部岩浆作用成矿与找矿重点实验室陕西西安 长安大学地球科学与资源学院陕西西安 中南大学地球科学与信息物理学院湖南长沙 中国地质大学资源学院湖北武汉 lijinchao0313@163.com 
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中文摘要:
      青海东昆仑地区近年来沟里金矿、五龙沟金矿等老矿区取得了新进展和新突破,到继续开发,黑海北等多个新矿区(点)取得新发现。本文分析了区域成矿条件和典型矿床,总结出东昆仑地区金矿床的主要控矿因素,认为该地区金矿床主要形成于海西期-印支期,其次为加里东期;岩浆活动为金矿床形成提供了成矿流体和成矿物质来源;北西西-北西向构造及次级构造控制了金矿体的展布。成矿分析表明,东昆仑地区具有良好的金矿床成矿潜力与找矿前景。
英文摘要:
      Recent years have seen continued development of the old gold deposits, such as Gouli and Wulonggou, as well as discovery of many new gold deposits including Heihaibei in the East Kunlun region of Qinghai Province. This paper analyzes the metallogenic conditions and typical deposits and summarizes the key ore-controlling factors in this area. It is considered that the Late Variscan to Indosinian is the main mineralized period of gold deposits in East Kunlun, followed by Caledonian. The magmatism provides ore-forming fluids and material sources for the formation of gold deposits. NWW-NW structure and secondary structures control the distribution of gold orebodies. Metallogenetic analysis suggests that there exist good metallogenetic conditions and prospecting potential for gold deposits in the East Kunlun region.
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