冀北槟榔沟银金多金属矿地质特征及成矿规律浅析

槟榔沟银金多金属矿床位于华北板块北缘冀北——辽西成矿区，具有良好的金银成矿区域地质条件，丰宁——隆化断裂直接控制了该区的岩浆岩与火山岩分布和一系列次级断裂构造的发育，形成了良好的金银成矿构造条件。通过对地层、构造、岩浆岩与成矿的关系综合分析，对矿床成矿规律提出了初步的认识，并建立了该矿床成矿模式，认为该矿床为浅成中低温热液蚀变岩型银金矿床。

Analysis on Geological characteristics and ore-forming regularityof Binlanggou silver-gold polymetallic deposit in the northern Hebei province

Binlanggou silver gold polymetallic deposit is located the northern margin of the North China plate - into a mine in western Liaoning, And Fengning-Longhua deep fracture directly controls the distributing of igneous rocks and volcanic rocks, and a series of sub-faults, forming favorable structural condition of gold mineralization. By the mining area formation, structure, igneous rocks and mineralization of the relationship between comprehensive analysis of the Deposits made a preliminary understanding of the law, and established a model of the deposit.That the deposit is a shallow rock type in low-temperature hydrothermal alteration silver-gold deposit.