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川西北马脑壳微细浸染型金矿床地质特征及矿床成因
引用本文:王可勇,姚书振,杨言辰,代军治.川西北马脑壳微细浸染型金矿床地质特征及矿床成因[J].矿床地质,2004,23(4):494-501.
作者姓名:王可勇  姚书振  杨言辰  代军治
作者单位:1. 吉林大学地球科学学院,吉林,长春,130061
2. 中国地质大学,湖北,武汉,430074
基金项目:国土资源部“九五”科技攻关项目(95-02-002)的资助
摘    要:文章在系统总结马脑壳微细浸染型金矿床地质特征、成矿时代的基础上。通过稀土元素及氢、氧同位素地球化学研究,分析了矿床成因。结果表明,马脑壳金矿床形成于印支晚期,其成矿物质来自围岩地层,岩浆流体参与了成矿作用,矿床为与岩浆活动有关的混合热液金矿床。

关 键 词:地质学  微细浸染型  矿床成因  成矿时代  马脑壳金矿床  川西北
文章编号:0258-7106(2004)04-0494-08

Geological Characteristics and Origin of Manaoke Fine_grained Disseminated Gol d Deposit in Northwestern Sichuan Province
Wang Keyong ,Yao Shuzhen ,Yang Yanchen and Dai Junzhi.Geological Characteristics and Origin of Manaoke Fine_grained Disseminated Gol d Deposit in Northwestern Sichuan Province[J].Mineral Deposits,2004,23(4):494-501.
Authors:Wang Keyong  Yao Shuzhen  Yang Yanchen and Dai Junzhi
Institution:Wang Keyong 1,Yao Shuzhen 2,Yang Yanchen 1 and Dai Junzhi 1
Abstract:Based on summarization of geological features of the Manaoke fine_grained disseminated gold deposit, the authors analyzed its genesis through an integrated study of Rb_Sr isochron dating of fluid inclusions in quartz of the main ore_forming stage, geochemistry of rare earth elements and isotopes of hydrogen and oxygen. The results show that the Manaoke gold deposit was formed in Late Indosinian epoch, that its ore_forming materials came from surrounding strata, and that magmatic activities were involved in the ore_forming process. It is a mixed hydrothermal gold deposit related to magmatic activities.
Keywords:geology  fine-grained disseminated type  origin of an ore deposit  metallogenic epoch  Manaoke gold deposit  northwestern Sichuan Province
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