贵州遵义丁台镍钼矿床岩、矿石特征及其成因初探  

Characteristics of Rock and Ore and Preliminary Analysis of Genesis in Dingtai Ni-Mo Deposit in Zunyi of Guizhou Province

作　　者：张梅江[1] 张双菊[1] 谭月 李明琴[1] 

机构地区：[1]贵州大学资源与环境工程学院,贵州贵阳550003 [2]贵州省地质调查院,贵州贵阳550005

出　　处：《贵州大学学报（自然科学版）》2011年第1期30-34,共5页Journal of Guizhou University:Natural Sciences

基　　金：国家自然科学基金项目(NO.46302001)

摘　　要：遵义丁台镍钼矿床产于松林穹窿西侧的下寒武统牛蹄塘组底部的黑色岩系中,矿体呈薄层及扁豆状产出,厚0.04-0.08 m,个别扁豆体厚达0.2 m左右。本文通过对矿区岩、矿石特征的研究,初步分析丁台镍钼矿床成因。Dingtai Ni-Mo deposit in Zunyi area occur in the west side of the Songlin dome.It is produced from the black shale series at the base of Niutitang Formation,lower Cambrian Series,the ore body shape to flaggy and lenticle and output of 0.04 to 0.08 m thick,individual lenticle 0.2 m thick.This paper analyses genesis of Dingtai Ni-Mo deposit from the characteristics of rock and ore.

关 键 词：镍钼矿床 岩、矿石特征 矿床成因 遵义丁台 贵州 

分 类 号：P618.63[天文地球—矿床学] P618.65[天文地球—地质学]