| 江西盛源盆地基本地质特征 |
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| 引用本文： | 张万良.江西盛源盆地基本地质特征[J].江西地质,1998,12(1):48-52. |
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| 作者姓名： | 张万良 |
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| 作者单位： | 核工业华东地质局２６５大队 |
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| 摘 要： | 盛源盆地是我国一个重要产铀盆地；盆地构造以断裂为主；早白垩世末的北东向、北西向断裂导致了盆地的形成，晚白垩世后的北北东向断裂使盆地发生形变。
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| 关 键 词： | 结构 构造 盛源盆地 江西 |
THE BASIC GEOLOGICAL FEATURES OF SHENGYUAN BASIN |
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| Zhang Wanliang.THE BASIC GEOLOGICAL FEATURES OF SHENGYUAN BASIN[J].Jiangxi Geology,1998,12(1):48-52. |
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| Authors: | Zhang Wanliang |
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| Abstract: | The Shengyuan basin is a major uranium-producing basin in China , structures in this basin are dominated by fractures ;the NE-and NW-striking fractures led to the formation of the basin at the end of the Early Cretaceous Period,while from the Late Cretaceous onward ,the NNE-striking fractures brought about the deformation of the basin |
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| Keywords: | configuration structure Shengyuan basin Jiangxi |
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