Sedimentary facies of the Lower Jurassic Sangonghe Formation and its relationship with uranium mineralization in Mengqiguer area of Yili Basin, Xinjiang
Chen Fenxiong1, 2, Nie Fengjun1, Zhang Chengyong1, Zhang Zhanfeng2
1 School of Earth Science,East China University of Technology,Nanchang 330013,Jiangxi; 2 Geologic Party No.216,CNNC,Urümqi 830011,Xinjiang
Abstract Mengqiguer deposit is a large sandstone type uranium deposit discovered in recent years in Yili Basin of Xinjiang. Baesd on the lithology,sedimentary structures,sedimentary sequence,outcrop description and profile comparison,we explained the conditions and mechanism of uranium mineralization of the Lower Jurassic Sangonghe Formation in the study area. It is suggested that the fan delta front facies is the main type of sedimentary facies,including underwater distributary channel,distributary interchannel,underwater crevasse splay etc.,while the river mouth bar is not developed. The influence of sedimentary microfacies on uranium mineralization in the study area is mainly manifested in four aspects:(1)The sand body connectivity provided the spale for ore-forming fluid migration. (2)The underwater distributary channel sand is the main factor controlling the oxidation zone. (3)The sand body variation caused by changes of sedimentary microfacies made the ore body wider,thicker and uranium grade increase. (4)The mudstone skylight caused by underwater crevasse splay is one of the key factors in crossflow forming.
Fund:; [Co-funded by National Basic Research Program of China (973 Program)(No.2015CB453002)and Integrated Exploration Program for Key Basic Geological Research Plan (No.12120114007601)]
Corresponding Authors:
Chen Fenxiong,born in 1972,is a Ph.D. candidade and senior research engineer. He is engaged in uranium geological exploration and research. E-mail: 216chenfenxiong@163.com.
Cite this article:
Chen Fenxiong,Nie Fengjun,Zhang Chengyong et al. Sedimentary facies of the Lower Jurassic Sangonghe Formation and its relationship with uranium mineralization in Mengqiguer area of Yili Basin, Xinjiang[J]. JOPC, 2016, 18(5): 833-842.
Chen Fenxiong,Nie Fengjun,Zhang Chengyong et al. Sedimentary facies of the Lower Jurassic Sangonghe Formation and its relationship with uranium mineralization in Mengqiguer area of Yili Basin, Xinjiang[J]. JOPC, 2016, 18(5): 833-842.
[1] 陈戴生,王瑞英,李胜祥. 1997. 伊犁盆地层间氧化带砂岩型铀矿成矿模式. 铀矿地质,13(6):327-335. [Chen D S,Wang R Y,Li S X. 1997. Metallogenic medel of the sandstone-type uranium deposits in interlayer oxidation zone of Yili basin. Uranium Geology,13(6):327-335] [2] 冯建辉,姜在兴. 2000. 伊犁盆地层序地层及沉积学研究. 山东东营:石油大学出版社. [Feng J H,Jiang Z X. 2000. Study of sequence stratigraphy and sedimentary of Yili basin. Shandong Dongying:Petroleum University Press. [3] 蒋宏,张占峰,刘铭艳. 2011. 伊犁盆地南缘某矿床构造与铀成矿关系. 新疆地质,29(3):327-331. [Jiang H,Zhang Z F,Liu M Y. The relationship between the structure and uranium mineralization in the souther of Yili basin. Xinjiang Geology,29(3):327-331] [4] 姜在兴. 2003. 沉积学. 北京:石油工业出版社. [Jiang Z X. 2003. Sedimentology. Beijing:Petroleum Industry Press] [5] 焦养泉,陈安平,王敏芳,吴立群,原海涛,杨琴,张承泽,徐志诚. 2005. 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. 沉积学报,23(3):371-379. [Jiao Y Q,Chen A P;Wang M F,Wu L Q,Yuan H T,Yang Q,Zhang C Z. Xu Z C. 2005. Genetic analysis of the bottom sandstone of zhiluo formation,northeastern Ordos basin:Predictive base of spatial orientation of sandstone-type uranium deposit. Acta Sedimentologica Sinica,23(3):371-379] [6] 康勇,王冰. 2010. 伊犁盆地南缘蒙其古尔铀矿床越流补给成矿作用. 新疆地质,28(3):316-318. [Kang Y,Wang B. 2010. The more current supply of Mengqiguer uranium ore deposits in southern margin of Yili basin. Xinjiang Geology,28(3):316-318] 李宝新,陈永宏. 2010. 新疆伊犁盆地蒙其古尔地区层间氧化带成因分析. 四川地质学报,30(4):395-396,398. [Li B X,Chen Y H. 2010. A study of genesis of the interlayer oxidized zone in the mengqiguer region,Yili basin. Acta Geologica Sichuan,30(4):395-396,398] [7] 李宝新,徐建国,王冰,刘陶勇. 2008. 新疆伊犁盆地南缘新生代构造特征及其对砂岩型铀矿的控制作用. 新疆地质,30(3):297-300. [Li B X,Xu J G,Wang B. 2008. The structure characteristic of cainozoic era to control sandstone uranium action in south Yili basin in Xinjiang. Xinjiang Geology,30(3):297-300] [8] 李盛富,颜启明,王新宇,张中旺,齐军让. 2006. 伊犁盆地水西沟群冲积扇—扇三角洲沉积体系研究. 新疆地质,24(3):297-304. [Li S F,Yan Q M,Wang X Y,Zhang Z W,Qi J R. 2006. Research on the depositional system of alluvial fans and fan-deltas of the shuixigou group in the south Yili basin,Xinjiang. Xinjiang Geology,24(3):297-304] [9] 李胜祥,韩效忠,蔡煜琦,郑恩玖,王保群. 2006. 伊犁盆地南缘西段中下侏罗统水西沟群沉积体系及其对铀成矿的控制作用. 中国地质,33(3):582-590. [Li S X,Han X Z,Cai Y Q,Zheng E J,Wang B Q. 2006. Depositional system of the lower-middle Jurassic shuixigou group in the western segment of the southern margin of the Yili basin and its controls on uranium mineralization. Geology in China,33(3):582-590] [10] 李细根. 2002. 伊犁盆地南缘乌库尔其矿区砂岩型铀矿化特征及控矿因素. 铀矿地质,18(1):28-35. [Li X G. 2002. Characteristics of sandstone-type uranium mineralization and ore-controlling factors in Wukurqi ore district at southern margin of Yili basin,Xinjiang. Uranium Geology,18(1):28-35] [11] 刘陶勇,毛永明. 2006. 新疆伊犁盆地南缘水西沟群沉积体系演化与赋铀性研究. 新疆地质,24(1):64-66. [Liu T Y,Mao Y M. 2006. Study on the evolution of sedimentation system and uranium-containing attribute of shuixigou group in south Yili basin in Xinjiang. Xinjiang Geology,24(1):64-66] [12] 秦明宽. 1997. 新疆伊犁盆地南缘可地浸层间氧化带型砂岩铀矿床成因及定位模式. 北京:核工业北京地质研究院. [Qin M K. 1997. Genesis and positioning mode of in situ leachable interlayer oxidation zone sandstone type uranium deposits in southern margin of Yili basin,Xinjiang. Beijing:Beijing Research Institute of Uranium Geology] [13] 王芳霞,罗星刚. 2012. 蒙其古尔矿床层间氧化作用及其成因. 中国核学会铀矿地质分会、中国核学会铀矿冶分会. 全国铀矿大基地建设学术研讨会论文集:469-504. [Wang F X,Luo X G. 2012. Interlayer oxidation and genesis analyse of Mengqiguer uranium deposit.Chinese nuclear uranium geology branch,China nuclear society of uranium mining and metallurgy branch. Conference proceedings on the construction of the national uranium mining:469-504] [14] 王星星,朱筱敏,宋爽,吴陈冰洁,贺敬聪,曹刚. 2016. 渤海湾盆地车西洼陷陡坡带古近系沙河街组沙三下段“源-汇”系统. 古地理学报,18(1):65-79. [Wang X X,Zhu X M,Song S,Wu C B J,He J C,Cao G. 2016. Source-to-sink system of the lower member 3 of Paleogene shahejie formation in steep slope zone of western Chezhen sub-sag,Bohai bay basin. Journal of Palaeogeography(Chinese Edition),18(1):65-79] [15] 王勋,蔡煜琦,张占峰,刘红旭,刘俊平. 2014. 蒙其古尔地区赋铀层沉积特征及其与砂岩型铀矿的关系. 铀矿地质,30(2):93-99. [Wang X,Cai Y Q,Zhang Z F,Liu H X,Liu J P. 2014. Relation of sedimentary characteristics of uranous strata to sandstone-type uranium mineralization in Mengqiguer area. Uranium Geology,30(2):93-99] [16] 吴仁贵,余达淦. 2005. 辫状沉积砂体与砂岩型铀矿的关系剖析. 铀矿地质,19(2):92-96,104 [Wu R G,Yu D G. 2005. Discussion on relationship between sandbody of braided stream channel sandstone-type uranium deposit. Uranium Geology,19(2):92-96,104] [17] 熊利平. 2003. 伊犁含油气盆地综合分析. 陕西西安:西北大学. [Xiong L P. 2003. Comprehensive analysis of Yili petroliferous basin. Shaanxi,Xi’an:Northwest University] [18] 张晓. 2012. 伊犁盆地南缘蒙其古尔铀矿床成因研究. 北京:核工业北京地质研究院. [Zhang X. 2012. Research on genesis of Mengqiguer uranium deposit in south Yili basin. Beijing:Beijing Research Institute of Uranium Geology] [19] 张占峰,蒋宏,王毛毛. 2010. 蒙其古尔铀矿床成矿驱动因素及其在伊犁盆地找矿实践中的意义. 矿床地质,S1:165-166. [Jiang H,Zhang Z F,Wang M M. 2010. The mineralization driving factors of Mengqiguer uranium deposit and its practice significance prospecting in Yili basin. Mineral Deposits,(S1):165-166]