方城县山头村银多金属矿矿床特征与成矿探讨

摘要

Shantou silver-polymetallic mine is located in SMNCB and eastward extension of the Funiu Mountain granite base. After a recent geological survey, we found the major ore body has obvious stratabound feature and performance of hot sedimentary mineralization, with comprehensive reflection of the early deposit of water jetsdeposition. Through geological survey of the silver polymetallic ore, the geological characteristics of the mine were seriously discussed in this paper.%方城县山头村银多金属矿区位于华北地块南缘和伏牛山花岗岩基东延部分，近年来地质调查工作发现，矿区主要矿体层控特征明显，具有热水沉积的成矿特征，综合反映为矿床早期具有热水喷流-沉积的成因特点。本文通过矿区银多金属矿的地质普查，对矿体形成的地质特征进行了探讨。