| 浙江199淋积矿床铀矿化类型及其特征 |
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| 引用本文： | 汤其韬.浙江199淋积矿床铀矿化类型及其特征[J].铀矿地质,2004,20(3):156-162. |
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| 作者姓名： | 汤其韬 |
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| 作者单位： | 浙江省核工业地质局269大队,浙江,金华,321028 |
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| 摘 要： | 本文论述了产于寿昌 梅城中生代火山喷发带的 1 99铀矿床的基本地质特征 ,在分析其矿化类型和控矿因素的基础上 ,探讨了矿床的成因 ,认为该矿床由淋积作用所形成。 1 99铀矿床具有品位高、埋藏浅、易于开采和浸出 ,经济效益较高的特点。
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| 关 键 词： | 铀矿化 淋积型 吸附还原剂 层间断裂 |
| 文章编号： | 1000-0658(2004)03-0156-07 |
| 修稿时间： | 2003年2月26日 |
Mineralization-type of uranium deposit No.199 and its characteristics |
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| TANG Qi-tao.Mineralization-type of uranium deposit No.199 and its characteristics[J].Uranium Geology,2004,20(3):156-162. |
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| Authors: | TANG Qi-tao |
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| Abstract: | Basic geologic characteristics of uranium deposit No.199 located in Shouchang-Meicheng Mesozoic volcanic-effusive belt are expounded.Meanwhile,on the basis of analyzing the mineralization type and ore-controlling factors,the genesis of the deposit is discussed.It is suggested that the deposit was formed by the infiltration process.Ores of uranium deposit No.199 are characterized by high grade,shallow occurrence,easiness to be mined and leached,as well as the high economic efficiency. |
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| Keywords: | uranium mineralization infiltration-type adsorbent-reductant interlayer fault |
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