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    内蒙古中东部上侏罗统满克头鄂博组划分及时代

    张永清

    张永清, 2021. 内蒙古中东部上侏罗统满克头鄂博组划分及时代. 地球科学, 46(1): 162-171. doi: 10.3799/dqkx.2020.248
    引用本文: 张永清, 2021. 内蒙古中东部上侏罗统满克头鄂博组划分及时代. 地球科学, 46(1): 162-171. doi: 10.3799/dqkx.2020.248
    Zhang Yongqing, 2021. Division and Age of the Upper Jurassic Mandetou Orbo Formation in Central and Eastern Inner Mongolia. Earth Science, 46(1): 162-171. doi: 10.3799/dqkx.2020.248
    Citation: Zhang Yongqing, 2021. Division and Age of the Upper Jurassic Mandetou Orbo Formation in Central and Eastern Inner Mongolia. Earth Science, 46(1): 162-171. doi: 10.3799/dqkx.2020.248

    内蒙古中东部上侏罗统满克头鄂博组划分及时代

    doi: 10.3799/dqkx.2020.248
    基金项目: 

    内蒙古区域地质调查片区总结与服务产品开发项目 121201130132001

    详细信息
      作者简介:

      张永清(1961-), 男, 高级工程师, 从事地质调查、矿产勘查及综合研究工作.E-mail:735629926@qq.com

    • 中图分类号: P534

    Division and Age of the Upper Jurassic Mandetou Orbo Formation in Central and Eastern Inner Mongolia

    • 摘要: 内蒙古自治区中东部满克头鄂博组以流纹质火山碎屑岩为主夹山间湖盆相陆相碎屑岩及少量流纹岩或英安岩.沉积岩中产叶肢介Magumbonia paramecia,Nestoria reticulate,N.xishunjingensis,N.cf.pissoui,Lioestheria sp.;双壳类Ferganoconcha curta,F.subcentralis,F.elongate;植物:Ginkgoites sp.,Cladophlebis sp.,Lycopodites sp.,Baiera gracilis,Phoenicopsis sp.化石.岩石化学SiO271.47%~75.96%,Ai2O312.50%~14.18%,K2O 3.84%~4.98%,Na2O 3.22%~4.14%,ALK 7.84%~9.12%,K2O>Na2O,显示高硅高碱特征;微量元素组成上以富集Rb、K、Th、U、La和LREE,亏损Ba、Nb、Sr、P和Ti为特征;稀土元素ΣREE=47.116×10-6~176.78×10-6,轻重稀土分溜明显,分溜系数(La/Yb)N为4.79~25.56,δEu为0.05~0.61,为中等铕负异常.4个样品在logδ-logτ图解上全部落入造山带山花岗岩区、Rb-Y+Nb图解上落在火山弧花岗岩区、Nb-Y图解上全部落入火山弧花岗岩同碰撞花岗岩区;在阿巴嘎旗-扎鲁特旗-巴林右旗一带采集了4个锆石LA-MC-IC-MS同位素,年龄值分别为138.89±0.93 Ma、137.70±1.40 Ma、147.70±1.20 Ma和137.27±0.96 Ma,将满克头鄂博组的时代置于晚侏罗世-早白垩世.

       

    • 图  1  大兴安岭中南段采样位置及区域地质略图

      Fig.  1.  Reginal geological sketch and sampling positions middle-south part Da Hinggan Mountains

      图  2  满克头鄂博组K2O-SiO2图解

      Peccerillo and Taylor(1976);横纵坐标的单位为%

      Fig.  2.  K2O-SiO2 diagram for specimens in Manketou'ebo Formation

      图  3  满克头鄂博组流纹岩原始地幔标准化微量元素蛛网图(a)和球粒陨石标准化稀土模式图(b)

      Fig.  3.  Primitive mantle normalized trace element spideriagrams for rhyolite (a) and chondrite-normalized REE pattern for rhyolite chondrite in Manketou'ebo Formation (b)

      图  4  满克头鄂博组被测锆石CL图像、LA-ICP-MS分析点及U-Pb谐和图

      Fig.  4.  CL images localities the points LA-ICP-MS measurements and the U-Pb concordia of zircons from the Manketou'ebo Formation

      图  5  满克头鄂博组构造判别图解

      Fig.  5.  Tectonic discrimination diagrams of the rhyolite in Manketou'ebo Formation

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