JOPC ›› 2016, Vol. 18 ›› Issue (5): 833-842. doi: 10.7605/gdlxb.2016.05.063

• PALAEOGRAPHY AND MINERAL RESOURCES • Previous Articles     Next Articles

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. 1 School of Earth Science,East China University of Technology,Nanchang 330013,Jiangxi;
    2 Geologic Party No.216,CNNC,Urümqi 830011,Xinjiang
  • Received:2015-05-25 Revised:2015-10-09 Online:2016-10-01 Published:2016-10-01
  • Contact: 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.
  • Supported by:
    ; [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)]

新疆伊犁盆地蒙其古尔地区下侏罗统三工河组沉积相及其与铀矿化的关系*

陈奋雄1, 2, 聂逢君1, 张成勇1, 张占峰2   

  1. 1 东华理工大学地球科学学院,江西南昌 330013;
    2 中核集团核工业二一六大队,新疆乌鲁木齐 830011
  • 作者简介:陈奋雄,男,1972年生,博士研究生,研究员级高级工程师,从事铀矿地质勘查及研究工作。E-mail: 216chenfenxiong@163.com。
  • 基金资助:
    *国家重点基础研究发展规划(973计划)(编号:2015CB453002)和整装勘查关键基础地质研究计划项目(编号:12120114007601)共同资助

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.

Key words: sedimentary microfacies, underwater distributary channel, cross flow, sandstone type uranium deposit, Jurassic, Yili Basin

摘要: 新疆伊犁盆地蒙其古尔矿床是近年来发现的大型砂岩型铀矿床。以下侏罗统三工河组为主要研究层位,通过岩性特征、沉积构造和沉积序列分析及露头描述和剖面对比,从沉积学的角度解释蒙其古尔矿区铀矿化的发育条件和成矿机制。研究认为,蒙其古尔地区三工河组以扇三角洲前缘沉积为主,水下分流河道、分流间湾、水下决口扇等为主要沉积微相类型,河口砂坝不发育。该沉积微相对研究区铀矿化的影响主要体现在4个方面:(1)砂体的连通性为成矿流体提供运移空间;(2)水下分流河道微相是控制氧化带发育及矿体富集程度的主要影响因素;(3)沉积微相变化导致的砂体变异部位是矿体厚度、宽度与富集程度增大的主要原因;(4)由决口扇形成的泥岩天窗是越流形成的关键因素之一。

关键词: 沉积微相, 水下分流河道, 越流, 砂岩型铀矿, 侏罗系, 伊犁盆地

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