摘要
阳山大坪银铅多金属矿地表及浅部表现为岩浆热液型的成矿类型,通过对其地球化学特征、矿化蚀变特征、矿体特征及成矿控矿特征分析研究,认为岩浆热液成矿类型不是阳山大坪矿床的主矿体,主矿体为深部隐伏岩体接触带附近的矽卡岩型矿体。成矿类型的确定为后期的勘查提供了找矿方向。
The shallow ore body of Daping Pb-Zn polymetallic deposit in Yangshan county is the magmatic-hydrothermal type.Based on studying onthe geochemical characteristics,mineralization alteration features,ore body characteristics and orecontrolling features,we consider that the main metallogenic type of the Daping Ag-Pb-Zn polymetallic deposit in Yangshan county is not a magmatic-hydrothermal metallogenic deposit.However,the mian ore body is the skarn-type ore body,which is located near contact zone of a deep concealed pluton.The determination of metallogenic type will provide the prospecting direction for the later exploration.
作者
骆文轩
LUO Wen-Xuan(940 Team of Geological Organization for Non-Ferrous Metals of guandong,qingyuan gongdong 511500)
出处
《世界有色金属》
2018年第10期119-120,共2页
World Nonferrous Metals
关键词
阳山大坪
铅锌多金属矿
矽卡岩型
Daping in Yangshan County
Ag-Pb-Zn polymetallic deposit
Skarn type