天井源金矿区成矿地质特征及矿床成因浅析  

Metallogenic Geologic Characteris And Deposit Genesis Analysis Of Tianjingyuan Gold Field

作　　者：张雄[1,2] 刘伟[1] 汤玄[1] 

机构地区：[1]江西省地质矿产勘查开发局赣东北大队,江西上饶334000 [2]中国地质大学资源学院,湖北武汉430074

出　　处：《世界有色金属》2015年第12期85-88,共4页World Nonferrous Metals

摘　　要：天井源金矿区位于赣东北地区,地处扬子板块与华南板块对接带北侧。该区区域褶皱构造和断裂构造发育,成矿地质条件优越。本文在分析天井源金矿区成矿地质特征的基础上,对该区矿床成因进行了分析,最后指出了矿区找矿标志。Tianjingyuan gold field ,belonging to northeastern Jiangxi,locates in northern part of the junction betweenYangtze and South China plates. This area, where regional fold structure and faulted structure developed well, has superior ore-forming geological condition. The paper analyzes deposit genesis based on analysis of the metallogenic geologic characteristics of Tianjingyuan gold field,and points out the ore guide finally.

关 键 词：赣东北地区 天井源金矿区 成矿地质特征 矿床成因 找矿标志 

分 类 号：P618.41[天文地球—矿床学]