| 白面石矿田的铀成矿特征 |
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| 引用本文： | 张万良.白面石矿田的铀成矿特征[J].地质找矿论丛,2001,16(4):257-261. |
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| 作者姓名： | 张万良 |
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| 作者单位： | 核工业270研究所, |
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| 摘 要： | 白面石铀矿田产于NW向展布的白面石盆地中,由4个矿床1个矿点所组成,铀矿化主要受菖蒲组下岩段即“第一层岩”层位,贯入玄武岩与“第一层砂岩”内外接触带和基底花岗岩中的裂隙所控制,是贯入玄武岩,特别是石英斑岩活动的产物。
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| 关 键 词： | NW向构造 贯入玄武岩 石英斑岩 白面石矿田 铀矿床 成矿作用 |
| 文章编号： | 1001-1412(2001)04-0257-05 |
| 收稿时间： | 2001/5/1 0:00:00 |
| 修稿时间： | 2001年5月1日 |
URANIUM MINERALIZATION CHARACTERISTICS OF THE BAIMIANSHI ORE FIELD |
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| ZHANG Wan-liang.URANIUM MINERALIZATION CHARACTERISTICS OF THE BAIMIANSHI ORE FIELD[J].Contributions to Geology and Mineral Resources Research,2001,16(4):257-261. |
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| Authors: | ZHANG Wan-liang |
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| Institution: | Research Institute No.270, Nuclear Industry, Nanchang 330200, China |
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| Abstract: | Baimianshi ore field, occurred in the Baimianshi basin which trends in NW, consists of four deposits and one occurrence. The orebodies, situated in the low part of the Chengpu formation, are governed by the "first sandstone layer" and the cranny of basement granite, Uranium mineralizations were the products of intruded basalt and quartz-porphyry activity. |
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| Keywords: | NW structure intruded basalt quartz-porphyry Baimianshi ore field uranium ore |
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