摘要
通过对三道沟银铅矿床区域地质背景、矿区地质特征和矿体特征的研究,认为矿床的形成受控于太华群地层、NE-NNE向的断裂构造以及燕山期的岩浆活动。区内各种成矿地质条件有利于成矿,对含矿构造破碎带C29、C3号应进一步控制。
It is believed that the formation of the Sandaogou silver-lead deposit was controlled by Dahua group strata, NE-NNE trending fracture zone and Yanshanian magmatic activities, based on the research on regional geological background, ore field geological characteristics and orebody characteristics of the deposit. Various ore-forming conditions in the region are favourable for mineralization, the ore bearing # C29 and C3 should be further prospected.
出处
《矿产与地质》
2011年第5期365-370,共6页
Mineral Resources and Geology
关键词
银铅矿床
地质特征
找矿方向
三道沟
silver-lead deposit, geological characteristics, prospecting direction, Sandaogou
