| 湘西北钒矿床地质特征及其成因 |
| |
| 引用本文： | 鲍正襄,万溶江,鲍珏敏.湘西北钒矿床地质特征及其成因[J].资源环境与工程,1998(2). |
| |
| 作者姓名： | 鲍正襄 万溶江 鲍珏敏 |
| |
| 作者单位： | 湖南地质矿产勘查开发局405地质队 |
| |
| 摘 要： | 湘西北钒矿床产于下寒武统木昌组底部或下部。矿体呈层状，产状稳定。矿石主要由水云母（伊利石）和硅质组成，并含有机质及藻类化石等。钒矿的形成与海底热水沉积及生物化学沉积作用密切相关。
|
| 关 键 词： | 湘西北 钒矿 地质特征 成因 |
GEOLOGICAL CHARACTERISTICS AND GENESIS OF THE VANADIUM DEPOSIT IN NORTHWESTERN HUNAN |
| |
| Bao Zhengxiang, Wan Rongjang, Bao Jueming.GEOLOGICAL CHARACTERISTICS AND GENESIS OF THE VANADIUM DEPOSIT IN NORTHWESTERN HUNAN[J].Resources Environment & Engineering,1998(2). |
| |
| Authors: | Bao Zhengxiang Wan Rongjang Bao Jueming |
| |
| Abstract: | With bedded ore body and stable attitude, the vanadium deposit in northwestern Hunan occures in the bottom and lower part of Muchang formation of Lower Cambrian Series in which the ores are mainly composed of hydromica(illite) and siliceous materials containing some organic materials and algaes. The genesis of the deposit is closely related to submarine hot-water sedimentary and biochemical-sedimentary. |
| |
| Keywords: | northwestern Hunan vanadium deposit geological characteristic genesis |
| 本文献已被 CNKI 等数据库收录！ |
