摘要
Taba金矿是近年马来半岛Sokor地区新发现的一小型金矿床,矿体产于二叠-三叠系火山-沉积岩系中,严格受近南北向断裂构造控制,普遍发育硅化、黄铁矿化、绢云母化、绿泥石化等围岩蚀变。描述了该矿床地质特征,总结了其主要控矿因素及矿化富集规律,并探讨了矿床成因。
Taba Gold Deposit is a small gold deposit newly discovered in Sokor area of Malay Peninsula in recent years. The orebody occurs in the Permian-Triassic volcanic-sedimentary rock series, strictly controlled by the nearly north-south faults, and generally develops wall rock alterations such as silicification, pyritization, sericitization and chloritization. This paper describes the geological characteristics of the deposit, summarizes its main ore-controlling factors and mineralization enrichment rules, and discusses the genesis of the deposit.
作者
邵立波
杨牧
邹海洋
SHAO Li-bo;YANG Mu;ZOU Hai-yang(Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring,Ministry of Education,Central South University, 410083, P.R. China;Hunan Key Laboratory of Nonferrous Resources and Geological Hazards Exploration in Hunan Province, 410083, P.R. China;School of Geosciences and Info-Physics,Central South University, 410083,P.R. China)
出处
《南方金属》
CAS
2019年第4期30-32,共3页
Southern Metals
关键词
地质特征
控矿因素
Taba金矿
马来半岛
geological characteristics
ore-controlling factors
Taba Gold Deposit
Peninsula of Malaysia