四川金阳热水河玄武岩型铜矿地质特征及找矿前景  

The Geological Characteristics and Prospecting Potential of Reshuihe Basalt Type Copper Depositin Jinyang,Sichuan Province

作　　者：唐军华 宋小琴 凌亚军 李俊 TANG Jun-hua;SONG Xiao-qin;LING Ya-jun;LI Jun(The 4th Geological Brigade of Sichuan,Chengdu 611130)

机构地区：[1]四川省第四地质大队,成都611130

出　　处：《四川地质学报》2023年第2期234-237,共4页Acta Geologica Sichuan

摘　　要：金阳热水河玄武岩型铜矿位于上扬子陆块东缘,四川前陆盆地筠连-叙永叠加褶皱带上,该矿是新发现的一处矿产地。笔者实地调查了该区基本地质概况,通过与乌坡式铜矿典型矿床成矿要素的对比,发现二者的成矿条件具极高的相似性,表明研究区玄武岩型铜矿成矿地质条件良好。同时结合该区地层、构造、矿化体等特征,预测该区玄武岩型铜矿具较好的找矿前景。The JinyangReshuihebasalt type copper deposit is located in the eastern margin of the Upper Yangtze block,Junlian-Xuyong superposition fold belt of Sichuan Foreland basin,which is a newly discovered orefield.Through the field investigation of the basic geological situation of this area and the comparison of metallogenic elements with typical copper deposits of the Upo type,it is found that the metallogenic conditions of the two have very high similarity,indicating that the basalt type copper deposit in the study area has good metallogenic geological conditions.Combined with the characteristics of strata,structure and mineralized body,it is predicted that the basalt type copper deposit has a good prospecting potential.

关 键 词：玄武岩型铜矿 地质特征 找矿前景 

分 类 号：P618.41[天文地球—矿床学]