阳春盆地庙山铜多金属矿床成矿模式探讨

Discussion on Metallogenic Model of Miaoshan Cu Polymetallic Deposit in Yangchun Basin

庙山矿区位于广东阳春盆地中部,属于岩浆热液有关的矽卡岩型矿床,近年来,通过地质勘查工作发现其矿床特征与邻近石菉矿床特征相似,推测靠近岩体尚有寻找接触带型乃至斑岩型铜多金属的巨大空间,通过进一步工作有望提交一处中型以上铜多金属矿产地。

The Miaoshan mining area is located in the middle of Yangchun Basin in Guangdong, belongs to the hydrothermal-related skarn deposits. Based on exploration work in the recent year and the comparative study about the similar geologic characteristics between Miaoshan Cu deposit and the adjacent Shilu ore cluster, it indicates that there are probably potential polymetallic orebody and porphyry copper deposits near contact zone of magmatic rock area. It is expected to be a medium or above copper deposit after further exploration.