| 敦煌方山口大型钒磷铀矿床的地质特征及成因 |
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| 引用本文： | 赵省民,聂风军,江思宏,白大明.敦煌方山口大型钒磷铀矿床的地质特征及成因[J].地球学报,2002,23(3):207-212. |
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| 作者姓名： | 赵省民 聂风军 江思宏 白大明 |
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| 作者单位： | 中国地质科学院矿产资源研究所，北京100037;中国地质科学院矿产资源研究所，北京100037;中国地质科学院矿产资源研究所，北京100037;中国地质科学院矿产资源研究所，北京100037 |
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| 基金项目： | 国家地质大调查项目(项目编号:K1.3.32) |
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| 摘 要： | 敦煌方山口大型钒磷铀矿床是一个多元素共生矿床，它既有与中国其它地区钒矿床相似之处，也有其自己独特的方面。研究该共生矿床的地质特征，阐明其中各种矿产的分布规律，查明其形成机制，以期在邻近地区寻找规模更大的钒、磷、铀矿床。
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| 关 键 词： | 铀钒磷矿床 地质特征 敦煌 |
Geological Features and Origin of the Fangshankou Large-scale V-P-U Deposit in Dunhuang, Gansu Province |
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| ZHAO Sheng-min,NIE Feng-jun,JIANG Si-hong and BAI Da-ming.Geological Features and Origin of the Fangshankou Large-scale V-P-U Deposit in Dunhuang, Gansu Province[J].Acta Geoscientia Sinica,2002,23(3):207-212. |
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| Authors: | ZHAO Sheng-min NIE Feng-jun JIANG Si-hong and BAI Da-ming |
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| Institution: | Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037;Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037;Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037;Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037 |
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| Abstract: | The Fangshankou V P U deposit, located in the north of Dunhuang City, Gansu Province,is a large scale deposit with multi element association. It shows some similarities to other vanadium deposits and also has its own distinctive qualities. The authors intend in this paper to study in detail geological features of the deposit and to make clear the distribution and formation of all kinds of mineral resources in it with the purpose of finding more vanadium, phosphorus and uranium resources in the surrounding areas and serving the development of West China. |
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| Keywords: | V-P-U deposit geological feature Dunhuang of Gansu province |
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