内蒙古维拉斯托锡多金属矿床含矿斑岩体钾长石斑晶的有序度及成因探讨
Geology and Resources（2017）
Abstract
钾长石有序度及结构温度可以为探讨成矿物化条件等提供依据.为阐明本区钾长石的成因,通过对维拉斯托斑岩体中钾长石斑晶的红外光谱分析,其有序度为0.85～0.95,三斜度为0.7～0.9,测定的结构温度为547.17～578.36℃,表明钾长石斑晶为微斜长石.并探讨了钾长石的成因,认为它是热液蚀变的产物.
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