| 512可地浸砂岩型铀矿床地质特征和远景评价 |
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| 引用本文： | 程明高 简晓飞. 512可地浸砂岩型铀矿床地质特征和远景评价[J]. 铀矿地质, 1995, 11(1): 11-18 |
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| 作者姓名： | 程明高 简晓飞 |
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| 作者单位： | 陕西西安核工业西北地勘局 |
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| 摘 要： | 本文介绍了５１２矿床区域地质背景、矿床基本特征、近期勘探成果、地浸效果和矿区远景评价。该矿床的成矿条件有利，属层间氧化带砂岩型，有可能发展成可地浸的、低品位的万吨级矿床，其矿田远景将更为可观。
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| 关 键 词： | 砂岩型，层间氧化带，地浸效果 |
GEOLOGICAL CHARACTERISTICS AND PROSPECTIVE ASSESSMENT OF IN-SITU LEACHING SANDSTONE TYPE URANIUM DEPOSIT |
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| Cheng Minggao, Jian Xiaofei. GEOLOGICAL CHARACTERISTICS AND PROSPECTIVE ASSESSMENT OF IN-SITU LEACHING SANDSTONE TYPE URANIUM DEPOSIT[J]. Uranium Geology, 1995, 11(1): 11-18 |
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| Authors: | Cheng Minggao Jian Xiaofei |
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| Abstract: | This paper introduces regional geological setting, basic characteristics of the deposit, therecent exploration progress, in-situ leaching effect and prospective assessment of the ore district in uranium deposit No. 512. Metallogenetic conditions for the deposit are favourable, belonging to interlayer oxidation zone sandstone type. It is possible to develop the deposit intoan in-situ leaching, low ore grade, 10-thousand-ton-class one, and the prospect of the ore fieldmay be more considerable. |
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| Keywords: | Sandstone type Interlayer oxidation zone In-situ leaching effect |
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