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新寨锡矿矿体呈似层状、透镜状赋存于中寒武统田蓬组第三段（∈2t3）中,矿体顺层产出,含矿围岩为石英云母片岩、绿帘石化矽卡岩。该锡矿床的形成与老君山燕山期花岗岩侵入关系密切,为层控岩浆期后热液矿床。
云南麻栗坡县新寨锡矿成因分析
【摘 要】
：
新寨锡矿矿体呈似层状、透镜状赋存于中寒武统田蓬组第三段（∈2t3）中,矿体顺层产出,含矿围岩为石英云母片岩、绿帘石化矽卡岩。该锡矿床的形成与老君山燕山期花岗岩侵入关系密
【机 构】
：
云南省有色地质局306队
【出 处】
：
云南地质
【发表日期】
：
2017年3期
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