摘要
四道沟金矿位于辽宁省丹东地区,是一个混合岩化热液层控矿床。矿体围岩为早元古界辽河群盖县组中部变质岩系。矿体与围岩界限不清楚。“Ω”状回曲构造直接控制着矿体和岩层的空间分布,而且金矿化主要位于“Ω”状回曲构造的走向褶曲核部。
Sidaogou gold deposit is locatedc in Dandong,Liaoning Province,which is a migmatic hydrothermal stratabound ore deposit.The host rocks of the ore bodies,the Gaixian Formation of Liaohe Group,are a medium grade metamorphosed rock of the Early Proterogoic.The boundaries between the ore bodies and the host rocks are not clearly seen.The Ω-type structures strictly control the special disctribution of the ore bodies and their host rocks.The gold mineralization is mainly in the core area of the dip folds of the Ω...
出处
《有色矿冶》
2005年第5期1-3,共3页
Non-Ferrous Mining and Metallurgy
关键词
构造控矿
成矿机理
Ω状回曲构造
找矿方向
structural cre-controlling
metallogenic mechanism
the Ω-type structures
ore-hunting orentation