| 鄂尔多斯盆地南部直罗—店头地区侏罗系直罗组沉积特征及铀成矿* |
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| 引用本文： | 王晓鹏,刘坤鹏,陈宏斌,龚斌利,于宏伟,龚奇福,韩迪.鄂尔多斯盆地南部直罗—店头地区侏罗系直罗组沉积特征及铀成矿*[J].古地理学报,2020,22(2):295-308. |
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| 作者姓名： | 王晓鹏 刘坤鹏 陈宏斌 龚斌利 于宏伟 龚奇福 韩迪 |
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| 作者单位： | 核工业二〇三研究所,陕西咸阳 712000 |
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| 基金项目： | *中国核工业地质局铀矿地质勘查项目(编号: 201524,201828-1,201913-4)和中核集团“龙腾2020”(编号: LTD1601-3)联合资助 |
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| 摘 要： | 鄂尔多斯盆地南部中侏罗统直罗组下段砂岩中已发现店头砂岩型铀矿床及多个铀矿点,但对于盆地南部直罗组沉积相研究较为薄弱,制约了砂岩型铀矿的进一步找矿工作。通过剖面实测、岩心编录,结合石油、煤炭、核工业地质钻孔资料,对鄂尔多斯盆地南部直罗—店头地区直罗组沉积特征进行精细刻画。在此基础上,探讨了沉积相与铀成矿的关系及下一步找矿方向。结果显示,直罗组下段砂体厚度30~65 m、砂地比在0.6~0.75之间,为砂质辫状河沉积。直罗组上段早期砂体厚度10~38 m、砂地比值在0.15~0.45之间,为曲流河沉积;直罗组上段沉积晚期研究区位于湖盆中心所在位置,为滨浅湖沉积。沉积环境、沉积相、辫状河河道交汇部位、砂体厚度、沉积物粒度及泥岩夹层对铀成矿具有重要控制作用。直罗组下段辫状河河道交汇或分叉部位应作为勘查重点,心滩亚相的含炭屑、黄铁矿砂质碎屑岩可作为铀矿化的找矿标志。
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| 关 键 词： | 沉积相 侏罗系 直罗组 砂岩型铀矿 鄂尔多斯盆地南部 直罗-店头地区 |
| 收稿时间： | 2019-07-14 |
Sedimentary characteristics of the Jurassic Zhiluo Formation and uranium deposits in Zhiluo-Diantou area,southern Ordos Basin |
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| Wang Xiao-Peng,Liu Kun-Peng,Chen Hong-Bin,Gong Bin-Li,Yu Hong-Wei,Gong Qi-Fu,Han Di.Sedimentary characteristics of the Jurassic Zhiluo Formation and uranium deposits in Zhiluo-Diantou area,southern Ordos Basin[J].Journal of Palaeogeography,2020,22(2):295-308. |
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| Authors: | Wang Xiao-Peng Liu Kun-Peng Chen Hong-Bin Gong Bin-Li Yu Hong-Wei Gong Qi-Fu Han Di |
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| Institution: | No.203 Research Institute of Nuclear Industry,Shaanxi Xianyang 712000,China |
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| Abstract: | Diantou uranium deposits and multiple uranium mineralization sites have been discovered in the sandstones in the lower member of the Jurassic Zhiluo Formation in the southern Ordos Basin. However, the study on the sedimentary facies of the Zhiluo Formation, which restricts the prospecting work of sandstone-type uranium deposits. Based on the outcrop measurements and drilling core cataloging, and combined with the geological drilling data of petroleum, coal, and nuclear industry, we have elaborated the sedimentary characteristics of the Zhiluo Formation in the Fuxian area. We have also combined uranium source, structure, post-alteration and other factors to explore the relationship between sedimentary faces and uranium metallogenic conditions in the study area. The study found that in the lower member of the Jurassic Zhiluo Formation, the thickness of the sand body is 30-65 m and sand ratio is 0.6-0.75. It is gravel and sandy braided river deposit. In the upper member of the Jurassic Zhiluo Formation, the thickness of the sand body is 10-38 m, and the sand ratio is 0.15-0.45 and is a meandering river deposit. The study area is located at the center of the lake basin and sedimentary facies is coastal shallow lacustrine in the upper member of the Jurassic Zhiluo Formation. Sedimentary environment, sedimentary facies, the intersection of braided river channels, sand body thickness, sediment particle size and mudstone interlayer play an important role in controlling uranium mineralization. The exploration of uranium deposits in the northern part of the deposit should focus on the intersection or bifurcation of the braided river channel in the lower part of the Zhiluo Formation. The charcoal- and pyrite-bearing sandstone of channel bar can be used as a prospecting indicator for uranium mineralization. |
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| Keywords: | sedimentary facies Jurassic Zhiluo Formation sandstone-type uranium deposit southern Ordos Basin Zhiluo-Diantou area |
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