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首页|期刊导航|地质通报|内蒙古苏尼特左旗恩格日音铀矿床Th地球化学特征及其对沉积环境的指示

内蒙古苏尼特左旗恩格日音铀矿床Th地球化学特征及其对沉积环境的指示OA北大核心CSTPCD

Geochemical characteristics of thorium and their sedimentary environment indication of Engeriyin uranium deposit in Sunid Left Banner,Inner Mongolia

中文摘要英文摘要

恩格日音铀矿床是近年来在二连盆地马尼特坳陷内新发现的砂岩型铀矿床.对苏尼特左旗恩格日音地区 31 个钻孔278 件岩石样品Th元素地球化学含量特征、分布和变化规律进行归纳、整理,分析了Th元素含量影响因素和指示意义.结果表明,研究区Th含量值为 3×10-6~99.9×10-6,加权平均值为 24.03×10-6,显示出Th含量较坳陷南部火山岩平均值富集的特征.沉积岩样品中Th含量值主要与沉积物源Th含量、沉积物分选强弱、粒度、透水性、吸附性强弱等有关,而与深度、沉积过程中新形成的含钍矿物、岩石U含量、氧化还原环境等无明显相关性.综合分析认为,陆相盆地边缘沉积岩中Th元素的特征和相对含量的空间分布规律研究,可用于识别沉积盆地的沉积物源、建立等时地层格架、划分沉积相带及砂体连通情况、判断古水流方向及恢复古河道展布.

Located in the Sunid Left Banner,the Engeriyin deposit is a newly discoveried sandstone-type uranium deposit.Though summarized the geochemical characteristics and distribution of thorium contents in 278 samples from 31 boreholes in Engeriyin area of Manite depression in Erenhot Basin,this paper analyzed the influencing factors and indicating significance of thorium content.The findings indicate that the thorium level in this region is higher than that of the volcanic rocks to the south of the Manite depression,ranging from 3×10-6 to 99.9×10-6 with a weighted average of 24.03×10-6.The primary determinants of thorium content in rock samples,as determined by data processing and analysis,are the source of the sediment,the distance and sorting of transportation,the granularity,the water permeability,and the adsorption strength of sedimentary rock,all of which affect the migration and differentiation of thorium-bearing minerals.Additionally,there is no discernible relationship with the uranium concentration,the redox reaction,sample depth,or newly generated thorium-bearing minerals during the deposition process.Numerical characterization and spatial distribution of Thorium in sedimentary rocks along the margins of terrestrial basins are useful for locating sedimentary sources within sedimentary basins,creating isochronous stratigraphic grids,defining sedimentary phases and sand connectivity,figuring out the direction of palaeocurrents,and reestablishing palaeochannel spreads.

蒋喆;韩效忠;胡航;来强;郭鹏;李紫楠

中国煤炭地质总局碳中和研究院,北京 100040||中国矿业大学资源与地球科学学院,江苏徐州 221116中煤地质集团有限公司,北京 100040

地质学

地球化学物源分析铀矿床内蒙古二连盆地

thoriumgeochemistryprovenance analysisuranium depositInner MongoliaErenhot Basin

《地质通报》 2024 (006)

926-937 / 12

中国地质调查局项目《内蒙古苏尼特左旗陆海地区铀矿地质调查》(编号:DD20190121-01)和中国煤炭地质总局科技项目《煤系矿产资源勘查开发关键技术研究》(编号:ZMKJ-2021-ZX03)

10.12097/gbc.2022.07.036

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