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    辽东本溪关门山岩体的年代学、地球化学及构造背景

    刘杰勋 李世超 朱凯 赵庆英

    刘杰勋, 李世超, 朱凯, 赵庆英, 2020. 辽东本溪关门山岩体的年代学、地球化学及构造背景. 地球科学, 45(3): 869-879. doi: 10.3799/dqkx.2019.064
    引用本文: 刘杰勋, 李世超, 朱凯, 赵庆英, 2020. 辽东本溪关门山岩体的年代学、地球化学及构造背景. 地球科学, 45(3): 869-879. doi: 10.3799/dqkx.2019.064
    Liu Jiexun, Li Shichao, Zhu Kai, Zhao Qingying, 2020. Geochronology, Geochemistry and Tectonic Setting of the Guanmenshan Pluton in Benxi, Eastern Liaoning Province. Earth Science, 45(3): 869-879. doi: 10.3799/dqkx.2019.064
    Citation: Liu Jiexun, Li Shichao, Zhu Kai, Zhao Qingying, 2020. Geochronology, Geochemistry and Tectonic Setting of the Guanmenshan Pluton in Benxi, Eastern Liaoning Province. Earth Science, 45(3): 869-879. doi: 10.3799/dqkx.2019.064

    辽东本溪关门山岩体的年代学、地球化学及构造背景

    doi: 10.3799/dqkx.2019.064
    基金项目: 

    国家自然科学基金项目 41872203

    国家自然科学基金项目 41872234

    详细信息
      作者简介:

      刘杰勋(1988-), 男, 博士研究生, 构造地质学专业

      通讯作者:

      李世超

    • 中图分类号: P588.12;P597.3

    Geochronology, Geochemistry and Tectonic Setting of the Guanmenshan Pluton in Benxi, Eastern Liaoning Province

    • 摘要: 在辽东中部的本溪-宽甸一带发育有较大规模的中生代岩浆岩,关于这些岩体的形成时代、岩浆来源及构造背景的研究相对滞后.本溪关门山岩体由花岗斑岩和碱长花岗岩构成,对其进行了岩石学、岩石地球化学及年代学研究.LA-ICP-MS锆石U-Pb定年结果表明,花岗斑岩侵位年龄为126.4±1.5 Ma,碱长花岗岩侵位年龄为125.7±1.7 Ma,形成于早白垩世.花岗斑岩和碱长花岗岩的主量元素具有富Si、K,贫Fe、Mg、Ca、Ti的特征,A/CNK=0.95~1.12;微量元素富集高场强元素K、Th、Rb,亏损Ba、Sr、Ti、P等;具有明显的负Eu异常,(La/Yb)N=7.62~17.32,轻重稀土元素分异明显.上述特征表明关门山岩体属于A型花岗岩.结合地球化学特征,关门山岩体为非造山的伸展构造背景下的岩浆活动产物,其受控于古太平洋板块向欧亚大陆俯冲的岩石圈减薄环境,是华北板块东部伸展地球动力学背景的具体体现.

       

    • 图  1  辽东本溪关门山地区地质简图(a)和中国东北构造地质简图(b)

      图b据杨凤超等(2018). 1.第四系;2.流纹质火山角砾凝灰岩;3.含煤地层;4古生界灰岩;5.青白口系石英砂岩;6.辽河群大理岩;7.花岗斑岩;8.碱长花岗岩;9.石英正长岩;10.霓霞正长岩;11.角度不整合;12.逆断层;13.性质不明断层;14.采样位置及编号

      Fig.  1.  Geological sketch of the Guanmenshan, eastern Liaoning Province (a) and tectonic map of Northeast China (b)

      图  2  研究区花岗斑岩和碱长花岗岩的宏观和显微特征

      a、b.花岗斑岩的野外照片及镜下特征;c、d.碱长花岗岩的野外照片及镜下特征. Q.石英;Pl.斜长石;Pth.条纹长石;Bi.黑云母

      Fig.  2.  Macro and Micro characteristics of granite porphyry and alkali-feldspar granite

      图  3  花岗斑岩(a)和碱长花岗岩(b)的锆石CL图像

      Fig.  3.  CL images of zircons from granite porphyry (a) and alkali-feldspar granite (b)

      图  4  花岗斑岩(a)和碱长花岗岩(b)的锆石LA-ICP-MS U-Pb年龄谐和图

      Fig.  4.  Concordia diagrams showing LA-ICP-MS zircon U-Pb ages for granite porphyry (a) and alkali-feldspar granite (b)

      图  5  花岗斑岩和碱长花岗岩的TAS图解(a)和SiO2-K2O图解(b)

      图a据Middlemost(1994)

      Fig.  5.  TAS (a) and SiO2-K2O (b) diagrams for granite porphyry and alkali-feldspar granite

      图  6  花岗斑岩和碱长花岗岩的球粒陨石标准化稀土元素配分模式(a)和原始地幔标准化微量元素蛛网图(b)

      标准化值分别据Boynton(1984)Sun and McDonough(1989)

      Fig.  6.  Chondrite-normalized REE pattern (a) and primitive mantle-normalized trace element spider diagram (b) for granite porphyry and alkali-feldspar granite

      图  7  花岗斑岩和碱长花岗岩的A型花岗岩判别图解

      a.底图据Whalen et al.(1987);b.底图据Eby(1992)

      Fig.  7.  Discrimination diagrams of A-type granites for granite porphyry and alkali-feldspar granite

      图  8  花岗斑岩和碱长花岗岩的构造环境R1-R2判别图(a)和(Y+Nb)-Rb判别图(b)

      R1= 4Si-11(Na+K)-2(Fe+Ti),R2= 6Ca+2Mg+Al

      Fig.  8.  R1-R2 (a) and (Y+Nb)-Rb (b) diagrams for granite porphyry and alkali-feldspar granite

      图  9  辽东半岛中生代构造-岩浆活动分布

      刘俊来等(2011)杨家林等(2018)

      Fig.  9.  Mesozoic tectonic-magmatic activity in the eastern Liaoning Province

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