| 湖北郧县大柳钒矿地质特征及成矿浅析 |
| |
| 引用本文： | 于洋,朱雪菡,秦林坡,杨华,李小迟.湖北郧县大柳钒矿地质特征及成矿浅析[J].安阳工学院学报,2012,11(4):69-71,113. |
| |
| 作者姓名： | 于洋 朱雪菡 秦林坡 杨华 李小迟 |
| |
| 作者单位： | 河南省有色金属地质矿产局第三地质大队,郑州,450000 |
| |
| 摘 要： | 郧县大柳钒矿赋存于下寒武统庄子沟组黑色岩系建造中,矿床属沉积成因。矿层呈层状、似层状,储量大,易勘查开发。成矿受地层、岩性、构造和古地理条件控制。
|
| 关 键 词： | 黑色岩系 地质特征 矿床成因 钒矿 大柳 |
The Geology and Formation of Vanadium Deposit in Yunxian County of Hubei Province |
| |
| YU Yang,ZHU Xue-han,QIN Lin-po,YANG Hua,LI Xiao-chi.The Geology and Formation of Vanadium Deposit in Yunxian County of Hubei Province[J].Journal of Anyang Institute of Technology,2012,11(4):69-71,113. |
| |
| Authors: | YU Yang ZHU Xue-han QIN Lin-po YANG Hua LI Xiao-chi |
| |
| Institution: | (Third Geological Party,Henan Exploration and Development of Geology and Mineral Resources,Zhengzhou 450000,China) |
| |
| Abstract: | Daliu vanadium deposit in Yunxian County lie at the black sequence of Lower Cambrian Zhuangzigou Formation,which is from sedimentation.The ore beds are stratified,stratoid,with large reserves and easily explored and developed.The metallogenesis is controlled by strata,lithology,structure and palaeoggraphic conditions. |
| |
| Keywords: | black sequence geology formation of deposit vanadium daliu |
| 本文献已被 CNKI 万方数据 等数据库收录！ |
|
