摘要
合肥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.
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)
关键词
镍钼矿床
岩、矿石特征
矿床成因
合肥丁台
贵州
Ni-Mo deposit
characteristics of rock and ore
deposit genesis
Dingtai area in Zunyi
Guizhou
