摘要
银屎铅锌矿床是玉水-银屎富铜多金属矿带中的一个典型矿床,矿体赋存于压扭性断裂破碎带中,多呈透镜状和脉状产出。综合其成矿地质背景、矿床地质特征等研究认为其矿床成因类型为热液裂隙充填和交代的后生层控矿床。
Yinshi Pb-zn deposit is in the Yushui-Yinshi excrement rich copper polymetallic ore belt,The orebody mainly occurs in the pressure-shear fracture zone and mostly lenticular and pulse output.According to its geological characteristics,of the deposit,we considered that it is a thermal fracture filling and metasomatic secondary control deposit.
作者
邓金龙
DENG Jin-long(The Guangxi Zhuang Autonomous Region Fourth Geological Team, Nanning 530051,China)
出处
《世界有色金属》
2018年第1期168-169,共2页
World Nonferrous Metals
关键词
地质特征
矿床成因
成矿模式
广东银屎
Geological characteristics
Deposit genesis
Metallogenic model
Guangdong Yinshi
