广西平垌岭地区钨矿床成矿地质条件分析  

Analysis on geological conditions of mineralization of tungsten deposits in Pingdongling region of Guangxi province

作　　者：刘运锷[1] 刘伟[1] 李莉[1] 陶明荣[1] 

机构地区：[1]中国有色桂林矿产地质研究院有限公司,广西桂林541004

出　　处：《矿产与地质》2012年第2期123-125,共3页Mineral Resources and Geology

摘　　要：平垌岭地区位于江南台背斜的西南端,为广西山字型构造系脊柱部分。沿区域性龙岸-元宝山大断裂由南向北分布有平垌岭一个大中型石英细脉带及大脉型钨矿床及雨累、九结、思英口、洞榕山等小型矿床(点),并构成了一小型钨矿田。Pingdongling region is located at southwest of the anticline of Jiangnan, which is the part of hack- bone of epsilon structural system of Guangxi. Along the large faults of regional Long＇an-Yuanbaoshan, there are a large-medium size quartz veinlet zone and large vein tungsten deposit in Pingdongling from the south to north, several mineral occurrence of tungsten in Yulei, Jiujie, Siyingkou etc. and they constitute a mine con- cession of tungsten.

关 键 词：钨矿床 成矿地质条件 平垌岭 广西 

分 类 号：P618.67[天文地球—矿床学]