湖北大冶市铜绿山铜铁矿地质特征及矿床成因  

THE GEOLOGICAL FEATURE AND GENESIS OF TONGLUSHAN CU-FE DEPOSIT IN DAYE,HUBEI

作　　者：邵显 Shao Xian(Tonglushan Mine of Daye Nonferrous Group Company(Ltd),China Nonferrous Group,Huangshi 435005)

机构地区：[1]中国有色集团大冶有色金属集团控股有限公司铜绿山矿,湖北黄石435005

出　　处：《云南地质》2021年第2期163-169,共7页Yunnan Geology

摘　　要：湖北大冶市铜绿山铜铁矿矿体呈透镜状、似层状产于花岗闪长斑岩体与下三叠统大冶组碳酸盐岩接触带附近,矿体形态与岩体与碳酸盐岩之接触带形态一致,矿体在平面上表现为一组出露深度不等的平行脉,剖面上呈雁行式斜列,具尖灭再现现象。该矿床成因类型为矽卡岩型铜铁矿床。The orebody in Tonglushan Cu-Fe deposit of Daye,Hubei is lenticular,stratoid near the contact between granodiorite porphyry and Lower T Daye Group carbonate rock.The orebody form consists with the contact between rock body and carbonate rock.The orebody is a set of parallel veins with different depth on the plane;whereas diagonal arrangement in the section,with thinning or reappear situation.It is a skarn u-Fe deposit in genesis.

关 键 词：矽卡岩矿床 接触带控矿 湖北大冶铜绿山 

分 类 号：P618.31[天文地球—矿床学] P618.41[天文地球—地质学]