从江污牙白钨矿地质特征及成因浅析  

Basic Geological Characteristics and Its Genesis of Wuya Scheelite Deposit in Congjiang

作　　者：潘光松[1] 胡桂敏[1] 

机构地区：[1]贵州省地质矿产勘查开发局105地质大队,贵州贵阳550018

出　　处：《贵州地质》2014年第4期286-290,共5页Guizhou Geology

摘　　要：从江污牙白钨矿,分布在吉羊穹状背斜北缘,赋存于摩天岭花岗岩外接触带甲路组一段下部的电气石—黑云母化石英千枚岩中。白钨矿的产出总是与特定的构造环境和蚀变特征联系在一起,并严格受其控制,本文试图从分析污牙白钨矿床的基本地质特征入手,探索该矿床的成因及指出下步找矿方向。Scheelite deposit in Congjiang distributs in north periclinal anticline in Jiyang, occurs in the tourmaline -aherationl quartz-phyllite of lower Jialu formation of outer contact zone of granite in Motianling. The output of Seheelite always has some connection with special structural environment and alteration, and be controlled strictly. In this paper, by discuss the basic geologic characteristics of Wuya scheelite deposit, it try to explore the genesis of the deposit and find out the prospecting direction in the future.

关 键 词：污牙 白钨矿 地质特征 成因 找矿方向 

分 类 号：P618.67[天文地球—矿床学]