摘要
本文提出了隆或金矿的成因与NE向断层密切相关,NE向断层最早可能为一条同生控相断层。所有已知矿床沿该断层分布,因此,北东向同生断层可能是隆或穹隆主要的控矿构造和流体通道,与隆或穹隆一起构成该区的一级控矿构造。综合分析了矿区成矿地质条件,为在矿区外围找矿提供了找矿标志,指出了找矿方向。
This paper puts forward that the genesis of Longhe gold deposit is closely related to NE trending fault,which may be a syngenetic facies fault at the earliest.All known deposits are distributed along the fault.Therefore,the NE trending syngenetic fault may be the main ore controlling structure and fluid channel of the uplift or dome,which together with the uplift or dome constitute the primary ore controlling structure in this area.This paper comprehensively analyzes the metallogenic geological conditions of the mining area,provides prospecting marks for prospecting in the periphery of the mining area,and points out the prospecting direction.
作者
陈忠斌
韦剑玮
CHEN Zhong-bin;WEI Jian-wei(The Fourth Geological Team of Guangxi Zhuang Autonomous Region,Nanning 530033,China)
出处
《世界有色金属》
2022年第9期64-66,共3页
World Nonferrous Metals
关键词
桂西隆林
隆或
金矿
同生控相断层
控矿构造
找矿标志
找矿方向
Guilin Longlin
Long or
gold mine
Syngenetic facies fault
Ore controlling structure
Prospecting marks
Prospecting direction
