摘要
乔夏哈拉金铜铁矿床产于中泥盆统北塔山组第三岩性段的一套海相火山岩、碎屑岩夹碳酸岩建造之中 ,金铜矿体的形成与后期的闪长 (玢 )岩的侵入所形成的夕卡岩密切相关 ,矿床成因为层控—夕卡岩型。
Qiaoxiahala gold-copper-iron deposit is hosted in the marine volcanic, clastic and carbonic rocks of No.3 section of the Beitashan group of middle Devonian. The formation of ore bodies is related with skarn which linked with the late diorite intrusion. The metallogensis of the deposit is stratabound skarn-type.
出处
《地质与勘探》
CAS
CSCD
北大核心
2002年第1期18-21,共4页
Geology and Exploration
