河北省涞水县交界口矿区多金属矿化特征及认识

Hebei Laishui junction of mining polymetallic mineralization characteristics and understanding

交界口矿区处于涞源-大河南北东向金-多金属成矿带上,是我部在2002年对该区进行1：5万路线地质调查过程中发现的金矿,通过近十年的地质工作,特别是利用岩石原生晕测量方法及有效的地表工程和深部钻探手段,大致查明了矿区具有以金为主的多金属（银、铅、锌、铜、钼、钛）成矿的地质特征。本文主要叙述了矿区内金、银、铜、铅、锌、钼、钛等主要成矿元素的成矿地质特征,并浅述了对矿区多金属矿化特征的认识,为今后工作提出了建议。

The junction of mine in Lai source-the river north and south trending gold-polymetallic metallogenic belt,is my portion of the zone in 2002,1：50,000 route gold discovered during geological survey,nearly a decade geological work,especially the use of native rock halo and effective methods of measurement of surface and deep drilling engineering means,generally identified with a gold mining area based multi-metal（silver,lead,zinc,copper,molybdenum,titanium）mineralization geological features.This paper describes the geological characteristics of the mineralization in the mining of gold,silver,copper,lead,zinc,mol ybdenum,titanium and other major ore-forming elements and said light for mining polymetallic mineralization characteristics of understanding,suggestions for future work.