贵州黄平上塘钒矿岩、矿石特征及其成因初探  

Characteristics of Rock and Ore and Preliminary Analysis of Genesis in Shangtang V Deposit in Huangping of Guizhou Province

作　　者：冉文瑞[1] 李明琴[2] 谢宏[2] 谢再波[2] 

机构地区：[1]贵州省国土资源勘测规划研究院,贵州贵阳550004 [2]贵州大学资源与环境工程学院,贵州贵阳550003

出　　处：《贵州大学学报（自然科学版）》2015年第4期27-30,共4页Journal of Guizhou University:Natural Sciences

基　　金：贵州省公益性;基础性地质勘察项目资助(黔财建[2011]114号)

摘　　要：黄平上塘钒矿产于下寒武统牛蹄塘组的黑色炭质粘土岩中,矿体严格受地层层位控制,呈层状、似层状产出,分为上、下两层,上层矿体产于牛蹄塘组中下部,平均品位较低,厚0.88-8.52 m,下层矿体产于牛蹄塘组底部,平均品位较高,厚1.00-26.47 m。本文通过对上塘钒矿区岩、矿石特征的研究,初步分析矿床成因。Shangtang V deposit in Huangping area is produced from the black anthrinoid clayrock of Niutitang Formation, lower Cambrian Series, the ore body is strictly controlled by horizon, a layered, stratified output, di- vide into upper and lower layers, the upper ore body is produced from middle to bottom of Niutitang Formation, a lower average grade, O. 88 to 8.52m thick, lower ore is produced from base of Niutitang Formation, a higher average grade, 1. 00 to 26.47m thick. This paper analyses genesis of Shangtang V deposit from the characteristics of rock and ore.

关 键 词：钒矿 岩、矿石特征 矿床成因 黄平上塘 贵州 

分 类 号：P611[天文地球—矿床学] P618.61[天文地球—地质学]