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凤翩山花岗岩类侵入体为一个中白垩世的小岩株(13km~2),产于山阳地带的钨成矿区。该岩体伴生有许多脉型铜矿床,矿化特征是除电气石外,还有多金属矿化(As、Co、Bi 和W)。岩株由云闪花岗闪长岩和花岗岩(出露
The granitic intrusions of Fenpishan are a small Cretaceous (13km ~ 2) in the Middle Cretaceous and are produced in the tungsten mineralization area of the Sanyang zone. The rock mass is associated with a number of vein-type copper deposits characterized by polymetallic mineralization (As, Co, Bi and W) in addition to tourmaline. The rock strain is composed of cloud-flash granodiorite and granite (exposed