浅析嵩山-侯家倒转背斜西翼“永平式”铜硫矿床

ON YONGPING - STYLED COPPER - SULFIDE DEPOSIT IN WEST SONGSHAN - HOUJIA INVERSED ANTICLINE

永平铜硫矿床位于嵩山-侯家倒转背斜的东翼,虽然矿化与矽卡岩化关系密切,成矿地质条件和成矿模式等都有别于一般的矽卡岩型矿床。鉴于矿床类型比较独特,专家和业内人士将矿床冠名为“永平式”铜硫矿床。嵩山-侯家倒转背斜的西翼,与永平铜硫矿床相比,具有相似的成矿地质环境,是寻找“永平式”铜硫矿床的重要“靶区”,找矿前景良好。

Yongping Cu - S deposit is located in the east of Shonshan - Houjia inversed anticline. Although its mineralization is closely related to scarnization, its mineralization geological condition and mode are deferent from normal scarn - type deposit. Due to the unique deposit category, it is named Yongping -style Cu -S deposit by experts and professionals in the area. In the west of Shongshan- Houjia inversed anticline, compared with Yongping Cu - S Deposit, possesses similar mineralization environment, is an important target for seeking Yongping - styled Cu - S deposit with good prospect for exploration.