| 松辽盆地南部协尔苏凹陷铀成矿控制因素与成矿模式探讨 |
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| 引用本文： | 席海银,王黎明,卢胜军,崔家瑞.松辽盆地南部协尔苏凹陷铀成矿控制因素与成矿模式探讨[J].国外铀金地质,2012(2):67-71. |
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| 作者姓名： | 席海银 王黎明 卢胜军 崔家瑞 |
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| 作者单位： | 核工业240研究所,辽宁沈阳110032 |
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| 摘 要： | 通过对协尔苏凹陷地质特征的研究，认为协尔苏凹陷铀矿（化）为后生多期次叠加改造成因，其形成主要受铀源、构造、目的层沉积体系、层间氧化带发育程度和地下水动力变异等因素控制。在总结上述控制因素的基础上，初步建立了成矿模式。
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| 关 键 词： | 松辽盆地南部 协尔苏凹陷 砂岩型铀矿 控制因素 成矿模式 |
Discussion on ore-controlling factors and metallogenic model of uranium ore-formation in Xieersu depression, south Songliao Basin |
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| Authors: | XI Hai-yin WANG Li-ming LU Sheng-jun CUI Jia-rui |
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| Institution: | (Research Institute No.240, CNNC, Shenyang, Liaoning 100023, China) |
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| Abstract: | Based on the geologic characteristics of Xieersu depression, uranium mineralization in this area is believed to be sandstone type of epigenie genesis of multi times superimposition and the ore-formation is mainly controlled by the factors such as the uranium source, the development of interlayer oxidation zone, the variation of hydrodynamic conditions, etc.. A preliminary metallogentie model has been set up. |
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| Keywords: | south So factors ngliao Basin metallogentic Xieersu depression sandstone-type uranium deposit ore-controlling model |
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