| 张振生,胡呈祥,张文昭.河南省庙咀钒矿地质特征及成矿浅析[J].地质找矿论丛,2014,29(2):217-222 |
| 河南省庙咀钒矿地质特征及成矿浅析 |
| Geological feature and genesis of Miaozui vanadium deposit in Xichuan county, Henan province |
| 投稿时间：2013-05-07 |
| DOI：10.6053/j.issn.1001-1412.2014.02.009 |
| 中文关键词: 庙咀钒矿 地质特征 矿床成因 找矿标志 河南省 |
| 英文关键词:Miaozui vanadium deposit geological feature genesis indicator for prospecting Henan Province |
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| 摘要点击次数: 1998 |
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| 中文摘要: |
| 庙咀钒矿是近年查明的一个中型钒矿床。钒矿床地处荆紫关—师岗复向斜南翼，矿体赋存于下寒武统水沟口组底部硅质岩和泥岩中，严格受控于地层及岩性。矿石类型主要为黏土岩型及条带状硅质岩型两种，钒主要以离子吸附和类质同象赋存于黏土矿物中。矿床成因为滨海-浅海沉积型层控矿床。 |
| 英文摘要: |
| Miaozui is a medium vanadium deposit located in the south flank of Jingziguan to Shigang synclinorium of the South Qinling fold belt. Ore bodies occur in black siliceous rock and mudstone at bottom of Lower Cambrian Shuikougou Formation and are strictly controlled by strata and lithologies. Clay rock and banded siliceous rock are the two main ore types. Vanadium occurs mainly as absorbed ions and isomorphs in clay minerals. Genetically it is a littoral-shallow sea stratabound sedimentary V deposit. |
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