| 吐哈盆地水文地质条件研究 |
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| 引用本文： | 谭鸿赞.吐哈盆地水文地质条件研究[J].铀矿地质,2002,18(2):97-103. |
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| 作者姓名： | 谭鸿赞 |
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| 作者单位： | 中国核工业地质局216大队，新疆乌鲁木齐，830011 |
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| 摘 要： | 铀成矿层间氧化带的形成，发育与地下水的形成演化密切相关，本文采用古水文地质的分析方法，对吐哈盆地地下水的演化史进行了研究，定量确定了地静压力系统和水静压力系统对沉积水的改造作用，计算了压挤水和渗入水的水交替强度，指出了铀成矿层间氧化带发育的有利地区。
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| 关 键 词： | 地静压力 水交替强度 层间氧化带 水文地质条件 吐哈盆地 铀矿床 |
| 文章编号： | 1000-0658(2002)02-0097-07 |
Study of hydrogeological conditions in Tulufan-Hami basin |
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| TAN Hong-zan.Study of hydrogeological conditions in Tulufan-Hami basin[J].Uranium Geology,2002,18(2):97-103. |
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| Authors: | TAN Hong-zan |
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| Abstract: | The formation,development of interlayer oxidation zone associated with uranium metallogenesis are closely related to the formation and the evolution of ground water.Applying the paleohydrogeologic analysis,this paper investigates the evolution history of groundwater in Tulufan-Hami basin,quantitatively determines the reworking process of terrestrial-static and water-static pressure systems on the sedimentation water,calculates the water-exchange intensity of squeeze water and infiltration water,and proposes the favourable areas for the formation of the development of interlayer oxidation zone associated with uranium metallogenesis. |
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| Keywords: | terrestrial-static pressure water-static pressure water-exchange intensity interlayer oxidation zone |
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