摘要
温杖子金矿位于青龙-锦西火山热液成矿带上,是一个典型的低温热液矿床。经多年开采,面临资源枯竭。结合实际勘查工作阶段性成果,对温杖子金矿外围地层、构造、岩浆岩、矿化蚀变、矿体特征进行分析研究,认为温杖子金矿外围的成矿条件和成矿模式与温杖子金矿类似,确定了找矿方向和找矿标志。
Wenzhangzi gold deposit is a typical low-temperature hydrothermal deposit located in the qinglong-Jinxi volcanic hydrothermal metallogenic belt.After years of exploitation,it is facing resource depletion.The strata,structures,magmatic rocks,mineralization alteration and orebody characteristics of the periphery of Wenzhangzi gold deposit are analyzed and studied based on the stage achievements of actual exploration work,it is considered that the metallogenic conditions and metallogenic model in the periphery are similar to that of Wenzhangzi gold deposit.
作者
张大伟
ZHANG Da-wei(Liaoning Nonferrous Geology 105 Team Co.,Ltd.,Huludao 125000,China)
出处
《有色矿冶》
2024年第2期1-3,6,共4页
Non-Ferrous Mining and Metallurgy
关键词
金矿
成矿条件
温杖子
gold mines
metallogenic conditions
Wenzhangzi
