赣中吉水银山—永丰白水地区黑色金属矿床地质特征及成因分析  

Geological characteristics and genetic analysis of black metal deposits from Jishui Yinshan to Yongfeng Baishui,central Jiangxi Province

作　　者：张栋梁 龙少秋 胡昊 ZHANG Dong-liang;LONG Shao-qiu;HU Hao(263 Brigade of the Jiangxi Nuclear Industry Geological Bureau,Nanchang 330096,China;Fourth Geological Team of Hubei Geological Bureau,Xianning 437100,China)

机构地区：[1]江西省核工业地质局二六三大队,江西南昌330096 [2]湖北省地质局第四地质大队,湖北咸宁437100

出　　处：《世界有色金属》2020年第16期184-185,共2页World Nonferrous Metals

摘　　要：本文在野外地质调查和前人资料研究基础上,通过对吉水银山、永丰九峰岭、永丰佐龙三个小型铁矿床地层划分、构造特征、矿层赋存形态与矿石类型及其变化等方面获得的勘查成果和认识,着重探讨铁矿床变质作用特征及成因。On the basis of field geological survey and previous data research,this paper focuses on the characteristics and genesis of metamorphism of iron deposits through the exploration results and understanding of stratigraphic division,structural characteristics,ore bed occurrence form,ore type and its change of three small iron ore deposits in Jishui Yinshan,Yongfeng jiufengling and Yongfeng Zuolong.

关 键 词：新余式铁矿 地质特征 矿床成因 

分 类 号：P618.2[天文地球—矿床学]