摘要
六道崴子铜矿床产于二叠系庙岭组大理岩与华力西晚期石英闪长岩接触部位,矿床因类型为接触交代型。
Liudaowaizi copper deposit occurs in the contact zone of the Miaoling Formation marble,in the Permian and quartz diorite in the late Variscan,which belongs to contact metasomatic deposit in types.
出处
《吉林地质》
2010年第4期32-34,共3页
Jilin Geology
关键词
铜矿床
地质特征
找矿方向
汪清六道
copper deposit
geologic features
prospecting direction
Liudao area of Wangqing