云南墨江金厂金矿床成矿特征和成矿作用  

Metallogenic characteristics and mineralization of Mojiang Jinchang gold deposit in Yunnan Province

作　　者：瞿剑飞 徐林刚[2] 王兵[1] 景辰 QU Jianfei;XU Lingang;WANG Bing;JING Chen(Xinjiang Vocational University Urumqi,Urumqi 830011,China;China University of Geosciences Beijing,Beijing 100083,China)

机构地区：[1]新疆职业大学,新疆乌鲁木齐830011 [2]中国地质大学(北京),北京100083

出　　处：《中国高新科技》2023年第15期109-111,共3页

摘　　要：墨江金厂金矿床是哀牢山金成矿带的重要矿床之一,具有独特的地质成矿特征。目前多个学者对墨江金矿床进行了研究工作,此矿床的成因是众多学者讨论的焦点。文章基于野外地质调查情况,根据矿床地球化学分析,对云南墨江金厂金矿床中成矿流体演化过程进行讨论,对成矿阶段做出明确的划分,并确定成矿流体来源,旨在深入了解此矿床的成因及成矿规律,为判断墨江金矿的成矿过程、矿床成因以及成矿阶段划分提供依据。Mojiang Jinchang gold deposit is one of the important deposits in Ailaoshan gold metallogenic belt,which has unique geological and metallogenic characteristics.At present,many scholars have studied the Mojiang gold deposit,and the genesis of this deposit is the focus of discussion.Based on the field geological survey and the geochemical analysis of the deposit,this paper discusses the evolution process of ore-forming fluid in the Mojiang Jinchang gold deposit,Yunnan Province,makes a clear division of the ore-forming stage,and determines the source of ore-forming fluid,in order to deeply understand the genesis and metallogenic law of this deposit,and provide the basis for judging the metallogenic process,deposit genesis and ore-forming stage of Mojiang gold deposit.

关 键 词：云南墨江金厂金矿床 成矿流体 矿体体征 成矿期次 

分 类 号：P618.51[天文地球—矿床学]