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    钱家店及外围红杂色含铀目标层位重新划分及其地质意义

    肖菁 秦明宽 郭强 严张磊 贾立城 刘鑫 邢作昌

    肖菁, 秦明宽, 郭强, 严张磊, 贾立城, 刘鑫, 邢作昌, 2024. 钱家店及外围红杂色含铀目标层位重新划分及其地质意义. 地球科学, 49(4): 1277-1291. doi: 10.3799/dqkx.2021.228
    引用本文: 肖菁, 秦明宽, 郭强, 严张磊, 贾立城, 刘鑫, 邢作昌, 2024. 钱家店及外围红杂色含铀目标层位重新划分及其地质意义. 地球科学, 49(4): 1277-1291. doi: 10.3799/dqkx.2021.228
    Xiao Jing, Qin Mingkuan, Guo Qiang, Yan Zhanglei, Jia Licheng, Liu Xin, Xing Zuochang, 2024. Red-Colored Uranium Target Horizon Reclassification and Its Significance in Qianjiadian Uranium Deposit and Surrounding Areas. Earth Science, 49(4): 1277-1291. doi: 10.3799/dqkx.2021.228
    Citation: Xiao Jing, Qin Mingkuan, Guo Qiang, Yan Zhanglei, Jia Licheng, Liu Xin, Xing Zuochang, 2024. Red-Colored Uranium Target Horizon Reclassification and Its Significance in Qianjiadian Uranium Deposit and Surrounding Areas. Earth Science, 49(4): 1277-1291. doi: 10.3799/dqkx.2021.228

    钱家店及外围红杂色含铀目标层位重新划分及其地质意义

    doi: 10.3799/dqkx.2021.228
    基金项目: 

    国防科工局核能开发项目 HSL1403

    详细信息
      作者简介:

      肖菁(1990-),女,博士,从事沉积地层、砂岩型铀矿地质研究工作. ORCID:0000-0002-6288-0328.E-mail:shawjingbao@sina.com

      通讯作者:

      郭强,E-mail: guoqiang9818@126.com

    • 中图分类号: P536

    Red-Colored Uranium Target Horizon Reclassification and Its Significance in Qianjiadian Uranium Deposit and Surrounding Areas

    • 摘要: 钱家店铀矿床及外围地区含矿目标层位划分不明已成为当前生产和科研迫切需要解决的关键问题.为准确厘定含矿层位,综合运用地层学、沉积学、砂岩型铀成矿理论,采取岩性、测井、古生物和其他多手段相结合的多重地层对比方法,系统分析了含矿目标层位的识别特征和划分依据.研究成果证明目前被统归划分为姚家组的含铀红杂色层可以识别并划分出泉头组、青山口组和姚家组,并在此基础上重新厘定了区域上不同矿体的层位归属和矿化特征.该研究可为松辽盆地南部铀矿勘查突破提供新的找矿思路和地质依据,在此新层位体系下进一步开展成矿规律研究,或许能真正有助于揭示长期以来悬而未决的板状铀矿体成因.

       

    • 图  1  研究区构造位置(a)及地质简图(b)

      图a审图号: GS(2019)1697号自然资源部监制

      Fig.  1.  Tectonic location (a) and geological sketch map (b) of research area

      图  2  地层识别方案示意图(图中照片详见图 3

      Fig.  2.  Schematic diagram of strata identifi1cation scheme

      图  3  目的层岩石学特征

      a.灰色泥岩,嫩江组,KT6;b.介形虫化石,深灰色泥岩,嫩江组,L7;c.叶肢介化石,灰色泥质粉砂岩,嫩江组,H16;d.紫红色泥砾岩,泉头组,S49;e.灰色-灰白色中砂岩,泉头组,S17;f.紫红色砂砾岩为主,青山口组底部,兴87;g.薄层灰色泥岩,青山口组顶部,兴105;h.灰白色中砂岩,姚家组,T6;i.灰色中-细砂岩,姚家组底部,T6;j.砖红色粉-细砂岩,姚家组,S33

      Fig.  3.  Petrological characteristics of target horizon

      图  4  目的层代表性孢粉——藻类化石

      1.希指蕨孢Schizaeoisporites;2.无突肋纹孢Cicatricosisporites;3.最小克拉梭粉ClassopollisminimusHerngreen;4.克拉梭克拉梭粉Classopollisclassoides;5.三角多环孢Polycingulatisporites triangularis;6.小桫椤孢Cyathidites;7.三花粉Nevesisporites;8.隐孔粉Exesipollenites;9.破隙杉粉Taxodiaceaepollenites hiatus;10.麻黄粉Ephedripites;11.美丽粉Beaupreaidites;12.拟千屈菜粉Lythraites;13.三角孢Deltoidospora;14.三孔孢Triporoletes;15.三孔沟粉Tricolpopollenites;16.网面三沟粉Retitricolpites;17.优美美丽粉Beaupreaiditeselegansiformis;18.单束松粉Abietineaepollenites;19.双束松粉Pinuspollenites;20.嫩江繁棒藻Cleistosphaeridiumnenjiangense;21.罗汉松粉Podocarpidites

      Fig.  4.  Representative palynological fossils and algal fossils of target horizon

      图  5  典型事件沉积构造现象

      a.微同沉积断裂,灰色含粉砂泥岩,s33;b.包卷层理,灰色泥质粉砂岩,s33;c.液化构造,灰色泥质粉砂岩,兴99;d.球枕构造,灰色泥质粉砂岩,兴99;e.火焰构造,灰色粉砂岩,兴105;f.角砾混杂堆积,灰色粉砂岩,兴105

      Fig.  5.  Typical structure of event sedimentology

      图  6  过各矿区典型钻孔连井剖面

      Fig.  6.  Profile of typical boreholes of through mining areas

      表  1  研究区地层划分方案

      Table  1.   Stratigraphic division scheme of study area

      松辽盆地南部 研究区地层划分 松辽盆地北部
      海力锦-钱家店-宝龙山 大林-双宝地区
      石油系统 铀矿系统 本次划分 石油系统 铀矿系统 本次划分
      嫩江组 嫩江组 嫩江组 嫩江组 嫩江组 嫩江组 嫩江组 嫩江组
      姚家组+青山口组 姚家组+青山口组 姚家组 姚家组 姚家组+青山口组 姚家组 姚家组 姚家组
      青山口组 青山口组 青山口组
      泉头组 泉头组 泉头组
      注:石油系统地层划分主要引自中国石油辽河油田内部报告:2012年《松辽盆地铀资源评价及南部地区铀成矿规律与预测研究》、2010年《钱家店凹陷上白垩统姚家组沉积特征及铀成矿地质条件研究》、2013年《内蒙古通辽市钱家店铀矿床外围详查地质报告》以及收集到的单井资料;铀矿系统地层划分主要引自核工业北京地质研究院内部报告:2015年《松辽盆地南部铀成矿条件评价及靶区优选》、2018年《蒙东-吉黑地区砂岩型铀矿成矿地质条件评价与远景预测》;核工业二四三大队内部报告:2015年《内蒙古通辽市宝龙山铀矿床及外围普查》和2015年《松辽盆地南部余粮堡-白城地区1∶25万铀矿资源区域评价》等.
      下载: 导出CSV

      表  2  松辽盆地前人孢粉化石研究

      Table  2.   Summary of previous studies on sporopollen fossils of Songliao basin

      研究范围 嫩江组 姚家组 青山口组 泉头组 文献来源
      松花江南部 被子植物花粉已占据重要地位,类型繁多 未发现孢子花粉 裸子花粉居优势,蕨类次之,被子花粉含量不超过10% 蕨类孢子和裸子花粉交替占优势 余静贤等(1983)
      松辽盆地 以大量发育多花孢和巴尔姆孢为特征 高瑞琪等(1988)
      松辽盆地新站地区 识别7个孢粉和藻类组合 田梦等(2005)
      松辽盆地青山口地区后金沟剖面 孢粉指示为嫩江组一段-二段下部 闫晶晶等(2007)
      开鲁盆地 蕨类、裸子、被子各站1/3 化石稀少 蕨类少于20%、裸子占75%、被子约6.4% 化石稀少 吴炳伟等(2007)
      姚家车站剖面 裸子占优势,蕨类和被子各具一定比例 化石稀少 席党鹏等(2009)
      松辽盆地东部五条剖面 识别出嫩三、四段3个孢粉组合 青一段1个组合,青二段2个组合,青三段1个组合 荆夏等(2011)
      钱家店凹陷1口井 建立3个孢粉组合,可对比 徐增连等(2017)
      钱家店凹陷12口井 裸子占优势,柏科和杉科花粉繁盛、三沟类发育 温国强等(2017)
      下载: 导出CSV

      表  3  典型样品绿鳞石化学元素组成定量分析表(%)

      Table  3.   Mineral component of green phosphorite in typical samples (%)

      样品号 Na2O SiO2 FeO CaO MgO Al2O3 TiO2 K2O MnO P2O5 总量
      S17-3 0.08 54.44 16.72 / 6.41 4.41 / 9.71 / / 91.77
      S49-6 / 53.57 17.01 / 3.74 6.43 0.05 10.08 0.04 0.04 90.96
      S33-2 0.08 54.88 14.80 / 6.71 5.12 0.09 9.85 0.05 91.58
      下载: 导出CSV
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    • 收稿日期:  2021-06-16
    • 网络出版日期:  2024-04-30
    • 刊出日期:  2024-04-25

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