摘要
伏牛山东麓地区经历了长期而复杂的构造演化,从新太古代到中生代、新生代不断活动,奠定了该区的基本构造格架。以成矿的大地构造背景为依据,结合已知金矿床(点)的分布和主要成因类型,将该区初步划分为黄土岭—郭沟、鸡冢—四里店、小东庄—夹山里沟3个成矿带,指出了不同区带主攻的矿床类型。
The tectonic evolution of the east foot of the Funiushan area has gone through long-term and complicated activities from Ptl to Mz and Cz, it forms the basic tectonics of this area. Based on the setting of the geo-tectonic, in respect of distribution of known deposits and its main genetic types, 3 mineralization zones have been divided in this area, namely Huangtuling-Guogou, Jicong-Silidian and Xiaodongzhuang- Jiashanligou ore belt. The target deposit types in the different districts are pointed out.
出处
《矿产与地质》
2005年第4期380-382,共3页
Mineral Resources and Geology
关键词
金矿床
找矿方向
综述
构造演化
成矿规律
伏牛山
河南
gold deposit, tectonic evolution, mineralization rule, exploration direction, FJaniushan, Henan
