摘要
从多期地壳演化、多期岩浆活动、多期断裂作用、多期固岩蚀变、多种矿石类型和多种矿化作用等方面论述了小寺沟铜钼矿床的复成性和多期性特征。
This paper discusses the polygenetic and mutliphase characteristics of the Xiaosigou Cu-Mn deposit according to polyphase crustal evolution, magnatic activity, faulting, wallrock alteration, ore types and mineralization.
关键词
铜钼矿床
复成性
多期性
Cu-Mn Deposit
Polygenetic
Multiphase
Xiaosigou, Hebei
