摘要
通过区域地质背景、构造格局、构造递变序列、矿床地质特征及成因研究,论述了脑包沟-北召沟石英钾长石蚀变脉型金矿床的多源复成热液成因,并对研究区找矿前景进行了探讨。
The Naobaogou-Beizhaogou quartz K-feldspar altered vein type gold deposits of thepolygenic-complex hydrothermal genesis is reviewed, which draws support from the reglonal geologicsetting, tectonic framework, tectonic graded succession, character and genesis of mineral deposits.Lastly, the prospecting foreground in study area is discussed.
出处
《西北大学学报(自然科学版)》
CAS
CSCD
北大核心
1997年第1期79-84,共6页
Journal of Northwest University(Natural Science Edition)
基金
内蒙古有色地质勘探局资助
关键词
构造格局
金矿床
成因
地质特征
tectonic framework
quartz K-feldspar altered vein type gold deposit
NaobaogouBeizhaogou district