| 张太富,谢兴友,张伍林.江口盘坡钒矿床地质特征及成因分析[J].贵州地质,2016,33(1):44-49 |
| 江口盘坡钒矿床地质特征及成因分析 |
| Geological Characteristics and Genesis Analyses of Panpo Vanadium Deposit in Jiangkou |
| |
| DOI： |
| 中文关键词: 钒矿 地质特征 矿床成因 |
| 英文关键词:Vanadium deposit Geologic characteristics Deposit genesis |
| 基金项目: |
|
| 摘要点击次数: 608 |
| 全文下载次数: 496 |
| 中文摘要: |
| 江口盘坡钒矿产于寒武系下统九门冲组底部，矿体呈层状、似层状，矿石矿物主要成分有炭质、有机质、石英、白云母、绢云母、粘土矿物等。矿体严格受层位、沉积环境的控制，矿床成因为海相化学及生物化学沉积钒矿床。 |
| 英文摘要: |
| Panpo vanadium deposit located in the low Jiumenchong formation of lower Cambrian，the orebody is stratiform or stratiform like，the minerals include carbon，organic matter，quartz，muscovite，sericite，clay mineral and so on. The orebody is controlled by position，sedimentary environment，the deposit genesis is sea facies chemical and sedimentary chemical sedimentary vanadium deposit. |
| 查看全文 查看/发表评论 下载PDF阅读器 |
