摘要
介绍了良山铁矿区地层、构造、岩浆岩等矿区地质特征,通过对赣中铁矿田矿床成矿规律和典型矿区构造特征的认真研究,认为区内变质岩原岩主要形成于优地槽海底火山喷发环境,浅部与中深部是连续延伸,铁矿层相对稳定,保存较好。在二次褶皱构造的轴部及附近是铁矿赋存的有利构造部位。提出了"矿下找矿和寻找构造有利部位相结合"的找矿模式,并成功地在良山铁矿区中深部接替资源勘查实践中进行运用。
The author suggested the ore prospecting model of prospecting under ore couple with searching favorable sectors in this text which make successful application on exploration by serious research on metallogenic law of Iron mines in central Jiangxi and diggings tentoniccharacteristics at crisis mines substitute resource exploration of Liangshan Iron ore field. It will promote a new period of prospecting of iron ore in central Jiangxi at the medium deep.
出处
《东华理工大学学报（自然科学版）》
CAS
2013年第1期50-55,共6页
Journal of East China University of Technology(Natural Science)
关键词
铁矿
赣中铁矿田
中深部接替资源
成矿规律
找矿模式
iron ore
iron ore field in jiangxi
the deep successive resource
regularity of ore formation
mine exploration model
