| 绿色蚀变带的地球化学性质及其找矿意义探讨 |
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| 引用本文： | 丁万烈.绿色蚀变带的地球化学性质及其找矿意义探讨[J].铀矿地质,2003,19(5):277-282. |
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| 作者姓名： | 丁万烈 |
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| 作者单位： | 核工业208大队,内蒙古,包头,014010 |
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| 摘 要： | 鄂尔多斯盆地直罗组发育大规模的绿色蚀变带，目前对其地球化学性质及与铀矿化的关系在认识上存有分歧。笔经初步研究认为，绿色蚀变可能是热液还原作用的蚀变产物，它与铀矿化的关系密切，具有重要的找矿意义。
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| 关 键 词： | 绿泥石蚀变 热液还原作用 铀矿化 |
| 文章编号： | 1000-0658(2003)05-0277-06 |
| 修稿时间： | 2002年12月18 |
Geochemical character of green-color alteration and its prospecting significance |
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| DING Wan,lie.Geochemical character of green-color alteration and its prospecting significance[J].Uranium Geology,2003,19(5):277-282. |
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| Authors: | DING Wan lie |
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| Abstract: | Large scale green color alteration is developed in Zhiluo Formation,Ordos basin.At present,there is divergence of views in its geochemical character and relation to uranium mineratization.Having preliminarily studied the phenomenon,the author suggests that the green color alteration might be the product of hydrothermal reduction,and is closely associated with uranium mineralization,being of important prospecting significance. |
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| Keywords: | chlorite alteration hydrothermal reduction uranium mineratization |
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