| 吐哈盆地十红滩铀矿床构造特征及其与铀矿化时空关系研究 |
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| 引用本文： | 傅成铭,邱林.吐哈盆地十红滩铀矿床构造特征及其与铀矿化时空关系研究[J].新疆地质,2006,24(2):192-196. |
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| 作者姓名： | 傅成铭 邱林 |
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| 作者单位： | 1. 核工业203研究所,陕西,咸阳,712000
2. 新疆维吾尔自治区人民政府国家305项目办公室,新疆,乌鲁木齐,830000 |
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| 摘 要： | 在分析了十红滩矿床地质构造背景、主要断裂和褶皱构造特征的基础上,提出了吐哈盆地十红滩矿床具有断块构造活动的特点,并将该区划分为4个不同特点的断块区,论述了各断块构造的地质特征和对地下水及铀矿化的控制作用;将盆地演化与铀矿化划分为盆地基底形成、沉积建造形成、盆地改造及铀矿化3个大的阶段和若干次级阶段,指出了盆后构造对铀矿化的分布和矿体的产出状态有明显的控制作用.
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| 关 键 词： | 十红滩铀矿床 断块构造 构造演化与铀矿化 盆后构造控矿 |
| 文章编号： | 1000-8845(2006)02-192-05 |
| 收稿时间： | 09 5 2005 12:00AM |
| 修稿时间： | 12 14 2005 12:00AM |
STRUCTURAL CHARACTERISTICS, MINEROGENETIC RELATIONSHIPS AND SPATIAL DISTRIBUTION OF THE SHIHONHTAN URANIUM DEPOSIT,TURPAN-HAMI BASIN |
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| FU Cheng-Ming,QIU Lin.STRUCTURAL CHARACTERISTICS, MINEROGENETIC RELATIONSHIPS AND SPATIAL DISTRIBUTION OF THE SHIHONHTAN URANIUM DEPOSIT,TURPAN-HAMI BASIN[J].Xinjiang Geology,2006,24(2):192-196. |
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| Authors: | FU Cheng-Ming QIU Lin |
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| Institution: | 1.Research Institute No.203, CNNC, XianYang, Shanxi, 712000, China;2. No. 305 State Project Office of Xinjiang Uygur Autonomous Regional, Urumqi, Xinjiang, 830000 |
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| Abstract: | Analysis of geological structures and the characteristics of primary faults and folding at the Shihongtan uranium deposits indicate there was block-faulting in Shihongtan area. The area is divided into four block-faulting zones and the structural characteristics in each of the zones and the controlling factors affecting groundwater are discussed. The basin evolution and uranium mineralization are divided into three main stages, as well as several subsidiary stages. The clear controlling role basin structures on uranium ore distribution and morphology is described. |
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| Keywords: | Shihongtan uranium deposit block-faulting structure structure evolution and uranium mineralization ore-controlling role of basin structure formation |
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