| 侯兵德.贵州新场钒矿床地质特征及找矿远景分析[J].矿产勘查,2011,2(3):254-259 |
| 贵州新场钒矿床地质特征及找矿远景分析 |
| The geological characters and prospecting potential of Xinchang V deposit, Guizhou |
| 投稿时间：2010-09-08 |
| DOI： |
| 中文关键词: 钒矿 地质特征 贵州新场 |
| 英文关键词: V deposit geological characteristics Xinchang Guizhou |
| 基金项目: |
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| 中文摘要: |
| 新场钒赋矿层位于扬子沉积区东南缘斜坡环境中的坳陷盆地,含矿层位为寒武系下统九门冲组第一段下部,含矿岩性为炭质页岩、黏土岩,矿体呈层状、似层状,矿石矿物主要为碎屑物质、黏土矿物、炭质及沸石,受层位、岩性及沉积环境的控制,通过对矿床地质特征、成矿地质条件等综合分析,认为该矿床找矿远景具有较大的预期。 |
| 英文摘要: |
| The Xinchang V deposit is located in the depression basin, which is in the southeastern margin of Yangtze sediment area. The vanadium mineralization is hosted in Lower Cambrian Jiumenchong Fm. carbonaceous shale and claystone. The ore bodies occurring as stratified or like-stratified have ore minerals including clast, clays, carbon minerals and zeolite. The ore minerals are dominated by layer and sediment environment. It is suggested Xinchang deposit has a good potential for exploration on the basis of geological and mineralization characteristics. |
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