摘要
中庄-泽上金矿床隶属于牟平-乳山成矿带,区域成矿条件有利。该矿区已发现27条矿脉3条金矿体,围岩多发生绢英岩化、褐铁矿化、碳酸盐化,矿床类型为石英脉或蚀变岩+石英脉型。矿脉严格受断裂构造控制,北东东向断裂构造是该区找矿的突出标志,红褐色网脉状、褐色块状铁帽为该区找矿的直接标志。应加强对1、6号矿脉的综合研究和其他矿脉的查证工作。
Zhongzhuang and ZeShang gold deposit belongs to Muping - Rushan metallogenic belt with regionally favorable metallogenic conditions. The mining area has found 3 gold ore body in 27 veins, and occurred in surrounding rock are sericitization, limonitization, carbonation. The deposits type is quartz vein or altered rock ＋ quartz vein type. The veins are strictly controlled by the faults, and the NNE fault structure is remarkable signs of prospecting in this area, direct signs in the area are red brown stockwork, brown massive gossan ore prospecting. Comprehensive research on the No. 1 or No.6 vein axed the verification work of other veins should be strengthened.
出处
《甘肃冶金》
2015年第2期101-103,共3页
Gansu Metallurgy
关键词
金矿床
地质特征
矿床成因
中庄-泽上
gold deposits
geological characteristics
genesis
Zhongzhuang-Zeshang
