摘要
三板桥白钨矿床位于上扬子古陆块都龙变质核杂岩穹窿核部,目前矿区已发现白钨矿体4条,矿体呈层状或脉状产出,均赋存于矽卡岩带中,属岩浆矽卡岩型矿床。该矿床特征与长江中-下游多金属成矿区的层控矽卡岩型矿床相类似。
Sanbanqiao scheelite deposit is in the nuclear area of Dulong metamorphic nuclear complex of Upper Yangzi Oldland Massif. 4 scheelite bodies have been discovered in the orefield,which are bedded or veined,in the skarn zone,belonging to the magmatic skarn type deposit. The deposit feature is similar to the stratabound skarn type deposit of multimetallic metallogenetic area in middle-lower reaches of Changjiang River.
出处
《云南地质》
2017年第1期77-80,共4页
Yunnan Geology
基金
云南文山南温河穹窿地区地质矿产调查(编号:12120114078401)
