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机构地区:[1]河南省有色金属地质矿产局第三大队,河南镇平474250
出 处:《矿产与地质》2005年第4期380-382,共3页Mineral Resources and Geology
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.
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