黑龙江北师河一带地质成矿背景及成矿条件分析

The analysis of Heilongjiang Bei Shi River metallogenic background and metallogenic conditions

本区所处大兴安岭成矿带与小兴安岭张广才岭成矿带拼合处,矿体多赋存于花岗岩与老地层接触部位的变质岩中,且与本区成矿条件极为相似,区域上的多期次强烈的构造运动,使本区形成了众多控矿构造,是赋矿的有利部位和地质找矿的方向之所在。

This area is located in Greater Khingan Range metallogenic belt and small Xingan mountain zhangguangcai range metallogenic belt splice, ore bodies occur in the contact area of the old strata of granite and metamorphic rocks, and metallogenic conditions in this region is very similar to the regional multi period strong tectonic movement, the area has formed many control the ore structure, the ore favorable location and geological prospecting direction.