注溪钒矿床元素地球化学意义

金属矿山 ›› 2013, Vol. 42 ›› Issue (09): 108-112.

注溪钒矿床元素地球化学意义

杨恩林^1,2，吕新彪¹，陈焕²，吴波²

1.中国地质大学（武汉）资源学院；2.贵州地矿局117地质队

出版日期:2013-09-16 发布日期:2013-11-22
基金资助:
“十二五”国家科技支撑计划项目(编号：2011BAB06B04-05)，贵州地矿局地质科研项目（编号：200901）。

Element Geochemical Significance of Zhuxi Vanadium Deposit

Yang Enlin ^1,2，Lu Xinbiao¹，Chen Huan²，Wu Bo²

1.Faculty of Earth Resources，China University of Geosciences(Wuhan)；2.The Geological Team 117，Bureau of Geology and Mineral Exploration and Development of Guizhou Province

Online:2013-09-16 Published:2013-11-22

摘要/Abstract

摘要： 以贵州黔东地区注溪钒矿床为例，分析测试其矿石和围岩的主微量元素含量，讨论各种特征元素的含量和比值，结果表明样品δCe最大值和最小值分别对应钒的最低和最高含量；有氧、缺氧不断转变的海水环境致使九门冲组同一岩性段仅底部出现矿体；矿石中V呈多价态主要是因为南华狭窄洋底部由阶梯式断层组成；海水缺氧且有大量富含V元素的有机质导致钒富集成矿；被动大陆边缘、多次海平面升降旋回和氧化还原界面之下为钒矿床的古地理环境。

关键词: 注溪钒矿床, 古地理环境, 海平面旋回

Abstract: Taking Zhuxi vanadium deposit in the Qiandong area，Guizhou province as an example，the concentration of major and trace element of rocks and sandstone are analyzed and surveyed，and the contents and ratios of the characteristic elements are discussed.The results showed that the maximum and minimum δ Ce value of the sample correspond to the lowest and highest levels of vanadium respectively; seawater environment with aerobic-anoxic continuous changing results in forming ore bodies only at the bottom of Jiumenchong Group with the same lithologic section.V in ores shows in multivalent form mainly due to the ladder faults at the narrow ocean bottom of Nanhua.Hypoxic seawater with V-riched organic matter results in ore-forming of vanadium.Passive continental margin，repeatedly eustatic cycles and redox interface serve as ancient geographical environments for vanadium deposits.

Key words: Zhuxi vanadium deposit, Palaeo-geographic environment, Eustatic sea-level change

杨恩林, 吕新彪, 陈焕, 吴波. 注溪钒矿床元素地球化学意义[J]. 金属矿山, 2013, 42(09): 108-112.

YANG 恩Lin, 吕Xin-Biao , CHEN Huan, WU Bo. Element Geochemical Significance of Zhuxi Vanadium Deposit[J]. Metal Mine, 2013, 42(09): 108-112.

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