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[1]李瑞霜,刘战庆*,杨胜富.鄂尔多斯盆地东北部中侏罗统延安组地质特征及铀成矿条件[J].地球科学与环境学报,2020,42(06):833-848.[doi:10.19814/j.jese.2020.08010]
　LI Rui-shuang,LIU Zhan-qing*,YANG Sheng-fu.Geological Characteristics and Uranium Metallogenic Conditions of MiddleJurassic Yan'an Formation in the Northeastern of Ordos Basin, China[J].Journal of Earth Sciences and Environment,2020,42(06):833-848.[doi:10.19814/j.jese.2020.08010]
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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:
第42卷
期数:
2020年第06期
页码:
833-848
栏目:
非主题来稿
出版日期:
2020-11-15

文章信息/Info

Title:
Geological Characteristics and Uranium Metallogenic Conditions of Middle Jurassic Yan'an Formation in the Northeastern of Ordos Basin, China
文章编号:
1672-6561(2020)06-0833-16
作者:
李瑞霜1; 2; 刘战庆1*; 杨胜富2
1. 桂林理工大学 地球科学学院,广西 桂林 541004; 2. 核工业二〇八大队,内蒙古 包头 014010
Author(s):
LI Rui-shuang1; 2;  LIU Zhan-qing1*;  YANG Sheng-fu2
1. College of Earth Sciences, Guilin University of Technology, Guilin 541004, Guangxi, China; 2. No.208 Geological Party, CNNC, Baotou 014010, Inner Mongolia, China
关键词:
砂岩型铀矿;  地质特征;  延安组;  层间氧化带;  灰色砂体;  成矿条件;  伊盟隆起;  鄂尔多斯盆地
Keywords:
sandstone-type uranium deposit;  geological characteristic;  Yan'an Formation;  interlayer oxidation zone;  grey sandbody;  metallogenic condition;  Yimeng uplift;  Ordos Basin
分类号:
P619.14
DOI:
10.19814/j.jese.2020.08010
文献标志码:
A
摘要:
鄂尔多斯盆地是中国砂岩型铀矿的重要产区,赋矿岩层主要为中侏罗统直罗组下段砂岩层,其下部中侏罗统延安组研究程度较低,找矿成果不显著。对鄂尔多斯盆地东北部中侏罗统延安组沉积体系、砂体、层间氧化带、岩石矿物学及铀赋存形式等进行了系统分析。结果表明:延安组属于河流-三角洲沉积体系,自下而上可分为Ⅰ、Ⅱ、Ⅲ、Ⅳ、Ⅴ共5个岩段。其中,Ⅰ、Ⅴ岩段分别为辫状河相和曲流河相沉积的河道砂体,发育厚度大,透水性及连通性好,利于成矿; Ⅰ、Ⅴ岩段发育较好的层间氧化带,在氧化带前锋线附近有不同程度的铀矿化,并且铀矿化以微粒状、短柱状的铀石为主。综合分析铀矿物质来源、砂体、古气候、水文地质等条件,认为中侏罗统延安组具备铀成矿条件,尤其是Ⅰ、Ⅴ岩段氧化-还原过渡带中的灰色砂体具有较大成矿潜力。
Abstract:
Ordos Basin is an important production area of sandstone-type uranium deposits in China. The ore-bearing rocks are mainly sandstones in the lower section of Middle Jurassic Zhiluo Formation. The lower part of Middle Jurassic Yan'an Formation has a low degree of research, and the prospecting results are not significant. A systematic analysis of sedimentary system, sandbodies, interlayer oxidation zones, rock mineralogy and uranium occurrence forms of Middle Jurassic Yan'an Formation was carried out in the northeastern of Ordos Basin. The results show that Yan'an Formation belongs to the river-delta sedimentary system, and can be divided into five rock members of Ⅰ, Ⅱ, Ⅲ, Ⅳ and Ⅴ from bottom to top. Among them, Ⅰ and Ⅴ rock members are channel sandbodies deposited by braided river facies and meandering river facies with large thickness, good permeability and connectivity, and are conducive to mineralization; interlayer oxidation zones are well developed in Ⅰ and Ⅴ rock members. Different levels of uranium mineralization exist near the front line of oxidation zone, which is dominated by particulate and short columnar coffinite. Uranium mineral sources, sandbodies, palaeoclimate, hydrogeology and other conditions comprehensively show that Middle Jurassic Yan'an Formation has the uranium metallogenic conditions, especially the gray sandbodies in the redox transition zone of Ⅰ and Ⅴ rock members have large mineralization potential.

参考文献/References:

[1] 魏 东,马中豪,陈清石.鄂尔多斯盆地渭北隆起中—新生代构造特征及多种能源矿产共存关系[J].地球科学与环境学报,2016,38(3):355-364. WEI Dong,MA Zhong-hao,CHEN Qing-shi.Mesozoic-Cenozoic Structure Characteristics and Coexisting Relationships of Multiple Energy Minerals in Weibei Uplift of Ordos Basin[J].Journal of Earth Sciences and Environment,2016,38(3):355-364.
[2] 韩效忠,吴兆剑,林中湘,等.浅论中国北方主要产铀盆地含矿目标层沉积相对砂岩型铀矿的制约[J].大地构造与成矿学,2020,44(4):697-709. HAN Xiao-zhong,WU Zhao-jian,LIN Zhong-xiang,et al.Constraints of Sedimentary Facies of the Targeting Layers on Sandstone-type Uranium Mineralization in Major Uranium-producing Basins in Northern China:A Brief Disscussion[J].Geotectonica et Metallogenia,2020,44(4):697-709.
[3] 张天福,张 云,金若时,等.鄂尔多斯盆地东北缘侏罗系层序界面特征对砂岩型铀矿成矿环境的制约[J].中国地质,2020,47(2):278-299. ZHANG Tian-fu,ZHANG Yun,JIN Ruo-shi,et al.Characteristics of Jurassic Sequence Boundary Surfaces on the Northeastern Margin of Ordos Basin and Their Constraints on the Spatial-temporal Properties of Sandstone Uranium Mineralization[J].Geology in China,2020,47(2):278-299.
[4] 吴仁贵,陈安平,余达淦,等.沉积体系分析与河道砂岩型铀矿成矿条件讨论:以鄂尔多斯中新生代盆地东胜地区为例[J].铀矿地质,2003,19(2):94-99. WU Ren-gui,CHEN An-ping,YU Da-gan,et al.Analysis on Depositional System and Discussion on Ore-formation Conditions of Channel Sandstone Type Uranium Diposit:Taking Dongsheng Area,Ordos Meso-Cenozoic Basin as an Example[J].Uranium Geology,2003,19(2):94-99.
[5] 焦养泉,陈安平,王敏芳,等.鄂尔多斯盆地东北部直罗组底部砂体成因分析:砂岩型铀矿床预测的空间定位基础[J].沉积学报,2005,23(3):371-379. JIAO Yang-quan,CHEN An-ping,WANG Min-fang,et al.Genetic Analysis of the Bottom Sandstone of Zhiluo Formation Northeastern Ordos Basin:Predictive Base of Spatial Orientation of Sandstone-type Uranium Deposit[J].Acta Sedimentologica Sinica,2005,23(3):371-379.
[6] 李子颖,秦明宽,蔡煜琦,等.鄂尔多斯盆地砂岩型铀矿成矿作用和前景分析[J].铀矿地质,2020,36(1):1-13. LI Zi-ying,QIN Ming-kuan,CAI Yu-qi,et al.Metallogenic Models and Prospective Analysis of Sandstone-type Uranium Deposits in Ordos Basin[J].Uranium Geology,2020,36(1):1-13.
[7] 肖新建.东胜地区砂岩铀矿低温流体成矿作用地球化学研究[D].北京:核工业北京地质研究院,2004. XIAO Xin-jian.The Mineralization Geochemistry of the Low Temperature Fluid on the Dongsheng Sandstone Type Uranium Deposit[D].Beijing:Beijing Research Institute of Uranium Geology,2004.
[8] 苗培森,陈 印,程银行,等.中国北方砂岩型铀矿深部探测新发现及其意义[J].大地构造与成矿学,2020,44(4):563-575. MIAO Pei-sen,CHEN Yin,CHENG Yin-hang,et al.New Deep Exploration Discoveries of Sandstone-type Uranium Deposits in North China[J].Geotectonica et Metallogenia,2020,44(4):563-575.
[9] 林中湘.砂岩型铀矿找矿目标层识别技术研究[J].中国煤炭地质,2019,31(8):49-53. LIN Zhong-xiang.Study on Sandstone Type Uranium Deposit Prospecting Target Identification Technology[J].Coal Geology of China,2019,31(8):49-53.
[10] 薛 锐.鄂尔多斯盆地北部直罗组沉积特征及其与铀成矿关系[D].西安:西北大学,2017. XUE Rui.Sedimentary Characteristics of the Jurassic Zhiluo Formation in Northern Ordos Basin and Implications for Uranium Mineralization[D].Xi'an:Northwest University,2017.
[11] 张金带.我国砂岩型铀矿成矿理论的创新和发展[J].铀矿地质,2016,32(6):321-332. ZHANG Jin-dai.Innovation and Development of Mentallogenic Theory for Sandstone Type Uranium Deposit in China[J].Uranium Geology,2016,32(6):321-332.
[12] 张天福,张 云,程银行,等.利用露头、井震及地球化学综合厘定层序界面:以鄂尔多斯盆地东北缘侏罗系为例[J].煤田地质与勘探,2019,47(1):40-48. ZHANG Tian-fu,ZHANG Yun,CHENG Yin-hang,et al.Integrated Identification of Sequence Boundary Through Outcrop,Seismic with Logging and Geochemistry:A Case of Jurassic in Northeastern Margin of Ordos Basin[J].Coal Geology and Exploration,2019,47(1):40-48.
[13] 史 勇,贾有根.鄂尔多斯东胜矿区色连井田侏罗系延安组沉积相展布及演化[J].中国煤炭地质,2020,32(2):13-21. SHI Yong,JIA You-gen.Jurassic Yan'an Formation Sedimentary Facies Extension and Evolution in Selian Minefield,Dongsheng Mining Area,Ordos Basin[J].Coal Geology of China,2020,32(2):13-21.
[14] 崔春兰,李 斌,任玺宁,等.大柳塔煤矿活鸡兔井田侏罗系延安组高分辨率层序地层及聚煤规律研究[J].地质与勘探,2020,56(3):614-626. CUI Chun-lan,LI Bin,REN Xi-ning,et al.High-reso-lution Sequence Stratigraphy and Coal Accumulation Law of Jurassic Yan'an Formation in the Huojitu Minefield of the Daliuta Coal Mine[J].Geology and Exploration,2020,56(3):614-626.
[15] 朱 强,俞礽安,李建国,等.鄂尔多斯盆地东北部塔然高勒地区还原介质对砂岩型铀矿的控制[J].煤田地质与勘探,2018,46(6):11-18. ZHU Qiang,YU Reng-an,LI Jian-guo,et al.Control of Reducing Medium on Uranium Deposit of Sandstone in Tarangaole Area,Northeastern Ordos Basin[J].Coal Geology and Exploration,2018,46(6):11-18.
[16] 杨仁超,韩作振,柳益群,等.鄂尔多斯盆地东胜地区侏罗系煤与铀矿关系[J].地球科学与环境学报,2006,28(4):31-37. YANG Ren-chao,HAN Zuo-zhen,LIU Yi-qun,et al.Relationship Between Jurassic Coal Measures and Uranium Deposits in Dongsheng Area,Ordos Basin[J].Journal of Earth Sciences and Environment,2006,28(4):31-37.
[17] 宋焕霞,赵世煌,赵桂军,等.大营铀矿勘查中实物地质资料的开发利用:找矿思维的转变与创新[J].地质通报,2016,35(11):1895-1899. SONG Huan-xia,ZHAO Shi-huang,ZHAO Gui-jun,et al.Second-round Development and Utilization of the Geological Samples in the Prospecting for Daying Uranium Deposit:Change and Innovation of Prospecting Thinking[J].Geological Bulletin of China,2016,35(11):1895-1899.
[18] JAIRETH S,ROACH I C,BASTRAKOV E,et al.Basin-related Uranium Mineral Systems in Australia:A Review of Critical Features[J].Ore Geology Reviews,2015,76:360-394.
[19] 张 宾,刘红旭,丁 波,等.鄂尔多斯盆地北部巴音青格利—苏台庙地区中侏罗统直罗组下段沉积特征及其铀成矿意义[J].高校地质学报,2020,26(2):218-230. ZHANG Bin,LIU Hong-xu,DING Bo,et al.Sedimentary Characteristics of the Lower Member of the Zhiluo Formation in Middle Jurassic and Its Uranium Metallogenic Significance in Bayinqinggeli-Sutaimiao Area,Ordos Basin[J].Geological Journal of China Universities,2020,26(2):218-230.
[20] 马 宁.基于钻孔大数据的鄂尔多斯盆地东北缘砂岩型铀矿三维地质成矿分析[D].长春:吉林大学,2020. MA Ning.Three-dimensional Geological Mineralization Analysis of Sandstone-type Uranium Deposits in the Northeastern Margin of the Ordos Basin Based on Borehole Big Data[D].Changchun:Jilin University,2020.
[21] 黄世杰.层间氧化带砂岩型铀矿的形成条件及找矿判据[J].铀矿地质,1994,10(1):6-13. HUANG Shi-jie.Formation Conditions and Prospect-ing Criteria for Sandstone Uranium Deposit of Interlayered Oxidation Type[J].Uranium Geology,1994,10(1):6-13.
[22] 易 超,王 贵,李 平,等.鄂尔多斯盆地北部纳岭沟铀矿床铁物相特征及其成矿意义[J].地质学报,2019,93(2):470-486. YI Chao,WANG Gui,LI Ping,et al.Characteristics of the Ferrum Phases in the Nalinggou Uranium Depo-sit,Northern Ordos Basin,and Its Metallogenic Significance[J].Acta Geologica Sinica,2019,93(2):470-486.
[23] 张天福,孙立新,张 云,等.鄂尔多斯盆地北缘侏罗纪延安组、直罗组泥岩微量、稀土元素地球化学特征及其古沉积环境意义[J].地质学报,2016,90(12):3454-3472. ZHANG Tian-fu,SUN Li-xin,ZHANG Yun,et al.Geochemical Characteristics of the Jurassic Yan'an and Zhiluo Formations in the Northern Margin of Ordos Basin and Their Paleoenvironmental Implications[J].Acta Geologica Sinica,2016,90(12):3454-3472.
[24] 孙立新,张 云,张天福,等.鄂尔多斯北部侏罗纪延安组、直罗组孢粉化石及其古气候意义[J].地学前缘,2017,24(1):32-51. SUN Li-xin,ZHANG Yun,ZHANG Tian-fu,et al.Jurassic Sporopollen of Yan'an Formation and Zhiluo Formation in the Northeastern Ordos Basin,Inner Mongolia,and Its Paleoclimatic Significance[J].Earth Science Frontiers,2017,24(1):32-51.
[25] 王双明.鄂尔多斯盆地聚煤规律及煤炭资源评价[M].北京:煤炭工业出版社,1996. WANG Shuang-ming.Coal Accumulation Law and Coal Resource Evaluation in Ordos Basin[M].Beijing:China Coal Industry Publishing House,1996.
[26] 葛玉辉,孙春林,刘茂修.鄂尔多斯盆地东北缘延安组划分与对比[J].地层学杂志,2007,31(2):151-156,197. GE Yu-hui,SUN Chun-lin,LIU Mao-xiu.Stratigra-phic Division and Correlation of the Yan'an Formation in the Northeastern Margin of the Ordos Basin,China[J].Journal of Stratigraphy,2007,31(2):151-156,197.
[27] 梁积伟.鄂尔多斯盆地侏罗系沉积体系和层序地层学研究[D].西安:西北大学,2007. LIANG Ji-wei.Research on Sedimentary System and Squence Stratigraphy of the Jurassic in Ordos Basin[D].Xi'an:Northwest University,2007.
[28] 易 超,陈心路,李西得,等.鄂尔多斯盆地北东部古层间氧化带砂岩型铀矿成矿特征[J].铀矿地质,2015,31(增1):247-257. YI Chao,CHEN Xin-lu,LI Xi-de,et al.Metallogenic Characteristic of the Paleo-interlayer Oxidation Type Sandstone-hosted Uranium Deposits in Northeastern Ordos Basin[J].Uranium Geology,2015,31(S1):247-257.
[29] 罗晶晶,李艳青,庞 康,等.鄂尔多斯盆地大营砂岩型铀矿古层间氧化带地球化学特征[J].铀矿地质,2018,34(5):280-287. LUO Jing-jing,LI Yan-qing,PANG Kang,et al.Geochemical Characteristics of Paleo-interlayer Oxidation Zone in Daying Uranium Deposit in Ordos Basin[J].Uranium Geology,2018,34(5):280-287.
[30] 李子颖,陈安平,方锡珩,等.鄂尔多斯盆地东北部砂岩型铀矿成矿机理和叠合成矿模式[J].矿床地质,2006,25(增1):245-248. LI Zi-ying,CHEN An-ping,FANG Xi-heng,et al.Metallogenic Mechanism and Superimposed Ore Mo-del of Sandstone Type Uranium Deposits in Northeastern Ordos Basin[J].Mineral Deposits,2006,25(S1); 245-248.
[31] FOLK R L,ANDREWS P B,LEWIS D W.Detrial Sedimentary Rock Classification and Nomenclature for Use in New Zealand[J].New Zealand Journal of Geology and Geophysics,1970,13(4):937-968.
[32] 苗爱生,陆 琦,刘惠芳,等.鄂尔多斯盆地东胜砂岩型铀矿中铀矿物的电子显微镜研究[J].现代地质,2010,24(4):785-792. MIAO Ai-sheng,LU Qi,LIU Hui-fang,et al.Electronic Microscopy Study on the Uranium Minerals of Dongsheng Sandstone Type Uranium Deposit in Ordos Basin[J].Geoscience,2010,24(4):785-792.
[33] 苗爱生,陆 琦,刘惠芳,等.鄂尔多斯砂岩型铀矿床古层间氧化带中铀石的产状和形成[J].地质科技情报,2009,28(4):51-58. MIAO Ai-sheng,LU Qi,LIU Hui-fang,et al.Occurrence and Formation of Coffinite in Ancient Interlayer Oxidizing Zone of Sandstone Type U-deposit in Ordos Basin[J].Geological Science and Technology Information,2009,28(4):51-58.
[34] 巫声扬,王德生.川北陆相砂岩型铀矿床成岩与成矿过程中有机质对铀的富集作用[J].铀矿地质,1991,7(5):265-272. WU Sheng-yang,WANG De-sheng.Uranium Concentration by Organic Matter During Diagenesis and Mi-nerlization in the Continental Sandstone-type Uranium Deposit in North Sichuan[J].Uranium Geology,1991,7(5):265-272.
[35] 权志高.层间氧化带边界类型划分与铀成矿潜力评价[J].地质找矿论丛,2003,18(4):225-228. QUAN Zhi-gao.The Division of Interl Formation Oxi-dized Zone Margins and Appraise of the Uranium Minerogenic Capacity[J].Contributions to Geology and Mineral Resources Research,2003,18(4):225-228.
[36] 李子颖,方锡珩,陈安平,等.鄂尔多斯盆地北部砂岩型铀矿目标层灰绿色砂岩成因[J].中国科学:D辑,地球科学,2007,37(增1):139-146. LI Zi-ying,FANG Xi-heng,CHEN An-ping,et al.Genesis of Grey Green Sandstone in Target Bed of Sandstone Type Uranium Deposit in Northern Ordos Basin[J].Science in China:Series D,Earth Sciences,2007,37(S1):139-146.
[37] 赵瑞全,秦明宽,王正邦.微生物和有机质在512层间氧化带砂岩型铀矿成矿中的作用[J].铀矿地质,1998,14(6):338-343,379. ZHAO Rui-quan,QIN Ming-kuan,WANG Zheng-bang.Effect of Microorganism and Organic Matters on Sandstone Type Uranium Mineralizations in Interlayer Oxidation Zone in Deposit No.512[J].Uranium Geology,1998,14(6):338-343,379.
[38] 古勃金 H B,斯米尔诺夫 A A.水成铀矿床的找矿标志和预测基础[M].雷文高,译.北京:原子能出版社,1985. GUBURKIN H B,SMIRNOV A A.Prospecting Criteria and Prediction Basis of Hydrothermal Uranium Deposits[M].Translated by LEI Wen-gao.Beijing:Atomic Energy Press,1985.
[39] 郝伟林.东胜地区铀成矿古水动力条件研究[D].北京:核工业北京地质研究院,2006. HAO Wei-lin.Study on Paleohydrodynamic Conditions of Metallogenesis of Uranium Deposit in Dongsheng Area[D].Beijing:Beijing Research Institute of Uranium Geology,2006.
[40] 王敏芳,焦养泉,杨 琴,等.鄂尔多斯盆地东北部延安组铀异常与沉积体系的关系[J].现代地质,2006,20(2):307-314. WANG Min-fang,JIAO Yang-quan,YANG Qin,et al.Relationship Between Uranium Anomaly and Depositional System of Yan'an Formation,Northeast Margin of Ordos Basin[J].Geoscience,2006,20(2):307-314.
[41] 彭云彪.内蒙古东胜地区1:250 000铀矿资源评价[R].包头:核工业二〇八大队,2002. PENG Yun-biao.Evaluation of 1:250 000 Uranium Resources in Dongsheng Area,Inner Mongolia[R].Baotou:No.208 Geological Party,CNNC,2002.
[42] 陈戴生,刘武生,贾立城.我国中新生代古气候演化及其对盆地砂岩型铀矿的控制作用[J].铀矿地质,2011,27(6):321-326,344. CHEN Dai-sheng,LIU Wu-sheng,JIA Li-cheng.Paleo-climate Evolution in China and Its Control on the Metallization of Sandstone Type Deposit of Meso-Cenozoic Basins[J].Uranium Geology,2011,27(6):321-326,344.
[43] 吴仁贵,祝民强,余达淦,等.鄂尔多斯盆地北部底河道砂岩型铀矿地质特征[J].东华理工学院学报,2006,29(1):1-6. WU Ren-gui,ZHU Min-qiang,YU Da-gan,et al.Geological Characteristics of Basal-channel Sandstone-type Uranium Deposits in the Northern of Ordos Basin[J].Journal of East China University of Technology,2006,29(1):1-6.
[44] 丹契夫 В И,斯特列梁诺夫 Н П.外生铀矿床:形成条件与研究方法[M].姚振凯,译.北京:原子能出版社,1984. DENCHEV В И,STRELENOV Н П.Formation Conditions and Research Methods of Exogenic Uranium Deposits[M].Translated by YAO Zhen-kai.Beijing:Atomic Energy Press,1984.
[45] 苗爱生,焦养泉,常宝成,等.鄂尔多斯盆地东北部东胜铀矿床古层间氧化带精细解剖[J].地质科技情报,2010,29(3):55-61. MIAO Ai-sheng,JIAO Yang-quan,CHANG Bao-cheng,et al.Detailed Investigation of the Paleo-interlayer-oxidation Zone of Dongsheng Uranium Deposit in Northeastern Ordos Basin[J].Geological Science and Technology Information,2010,29(3):55-61.

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备注/Memo

备注/Memo:
收稿日期:2020-08-09; 修回日期:2020-10-13; 网络首发日期:2020-11-15投稿网址:http:∥jese.chd.edu.cn/
基金项目:国家自然科学基金项目(41702211); 中国核工业地质局地勘费项目(201503)
作者简介:李瑞霜(1993-),男,内蒙古包头人,桂林理工大学理学硕士研究生,E-mail:964840035@qq.com。
*通讯作者:刘战庆(1975-),男,陕西蒲城人,副教授,理学博士,博士后,E-mail:lzqgygcx2008@163.com。
更新日期/Last Update: 2020-12-20