黑龙江省萝北县大金顶子镍矿矿床地质特征及成因探讨  

The Ore Deposit Character and Formation Discussing of Dajindingzi Nickel Ore

作　　者：鲍明学[1] 赵洁心[1] 李云国[1] 

机构地区：[1]黑龙江省老柞山金矿,黑龙江萝北154625

出　　处：《有色矿冶》2007年第4期1-2,6,共3页Non-Ferrous Mining and Metallurgy

摘　　要：介绍了萝北县大金顶子镍矿的地质特征,通过对资料的分析,推测该矿可能是一硫化镍矿,突破了原以为是风化壳型矿床的观点,为该矿床的进一步勘查工作提出了新的思路。The geographic character of dajindingzi nickel ore was introduced in detail. The analysis showed that this ore was concluded to be nickelsulphide but not weathering shell deposit. A new idea for further exploiting the ore was pointed out.

关 键 词：镍 地质特征 矿床成因 

分 类 号：P612[天文地球—矿床学]