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    古元古代全球静寂期岩浆活动——以华北克拉通南缘中条山~2.3 Ga横岭关花岗岩为例

    段庆松 宋会侠 杜利林 任留东 耿元生 王建龙 黄智强 王彦斌 杨崇辉

    段庆松, 宋会侠, 杜利林, 任留东, 耿元生, 王建龙, 黄智强, 王彦斌, 杨崇辉, 2020. 古元古代全球静寂期岩浆活动——以华北克拉通南缘中条山~2.3 Ga横岭关花岗岩为例. 地球科学, 45(9): 3372-3385. doi: 10.3799/dqkx.2020.237
    引用本文: 段庆松, 宋会侠, 杜利林, 任留东, 耿元生, 王建龙, 黄智强, 王彦斌, 杨崇辉, 2020. 古元古代全球静寂期岩浆活动——以华北克拉通南缘中条山~2.3 Ga横岭关花岗岩为例. 地球科学, 45(9): 3372-3385. doi: 10.3799/dqkx.2020.237
    Duan Qingsong, Song Huixia, Du Lilin, Ren Liudong, Geng Yuansheng, Wang Jianlong, Huang Zhiqiang, Wang Yanbin, Yang Chonghui, 2020. The Magmatic Activity in Paleoproterozoic Global Magmatic Quiescence: Take the ~2.3 Ga Henglingguan Granites from Zhongtiao Mountains in the Southern North China Craton as an Example. Earth Science, 45(9): 3372-3385. doi: 10.3799/dqkx.2020.237
    Citation: Duan Qingsong, Song Huixia, Du Lilin, Ren Liudong, Geng Yuansheng, Wang Jianlong, Huang Zhiqiang, Wang Yanbin, Yang Chonghui, 2020. The Magmatic Activity in Paleoproterozoic Global Magmatic Quiescence: Take the ~2.3 Ga Henglingguan Granites from Zhongtiao Mountains in the Southern North China Craton as an Example. Earth Science, 45(9): 3372-3385. doi: 10.3799/dqkx.2020.237

    古元古代全球静寂期岩浆活动——以华北克拉通南缘中条山~2.3 Ga横岭关花岗岩为例

    doi: 10.3799/dqkx.2020.237
    基金项目: 

    国家自然科学基金项目 41572175

    国家自然科学基金项目 41772191

    中国地质调查局地质调查项目 DD20190370

    中国地质调查局地质调查项目 DD20190003

    详细信息
      作者简介:

      段庆松(1996-), 女, 在读硕士研究生, 岩石学、矿物学、矿床学专业, 主要从事前寒武纪地质研究.ORCID:0000-0002-5988-7107.E-mail:songzi543@sina.cn

      通讯作者:

      杨崇辉, E-mail:chhyang@cags.ac.cn

    • 中图分类号: P583

    The Magmatic Activity in Paleoproterozoic Global Magmatic Quiescence: Take the ~2.3 Ga Henglingguan Granites from Zhongtiao Mountains in the Southern North China Craton as an Example

    • 摘要: 在全球岩浆活动静寂期,人们在华北克拉通内相继识别出大量~2.3 Ga的地质体,对探讨华北克拉通古元古代地质演化过程具有十分重要的意义.选择中条山地区横岭关二长花岗岩进行了地球化学、锆石U-Pb年代学和Hf同位素研究.横岭关二长花岗岩LA-ICPMS锆石U-Pb年龄结果为2 308±12 Ma,代表岩体的形成时代.横岭关二长花岗岩高硅、高钾、高铝、富碱,贫钙、低钠和低钛,A/CNK主要集中在1.0~1.1之间,为高钾钙碱性偏铝-过铝质花岗岩系列.岩石的稀土元素含量相对高,轻重稀土元素分异强烈,并具有明显的Eu负异常.高场强元素Nb、Ta、Zr、Hf、U和大离子亲石元素Rb等相对富集,亏损V、Cr、Co、Ni等相容元素,具有I型花岗岩的特征.横岭关二长花岗岩锆石εHft)为0.52~6.24,平均值为2.06,单阶段和两阶段模式年龄分别为2 419~2 642 Ma和2 438~2 738 Ma.横岭关二长花岗岩具有同碰撞花岗岩的特征,推测来源于~2.5 Ga古老地壳岩石在挤压碰撞环境下的部分熔融,揭示了华北克拉通在古元古代全球岩浆静寂期并不静寂.

       

    • 图  1  华北克拉通~2.3 Ga地质体分布

      底图据Zhao et al.(2005)Zhai and Santosh(2011);~2.3 Ga年龄数据见附表1文献.图中简写含义:AL.阿拉善; CD.承德; DF.登封; EH.冀东; ES.胶东; FP.阜平; GY.固阳; HA.怀安; HL.贺兰山; HS.恒山; JN.集宁; LL.吕梁; MY.密云; NH.冀北; QL.千里山; NL.辽北; SJ.吉南; SL.辽南; TH.太华; WD.乌拉山-大青山; WH.五河; WL.辽西; WS.鲁西; WT.五台; XH.宣化; ZT.中条

      Fig.  1.  The distribution map of ~2.3 Ga geologic bodies in the North China Craton

      图  2  华北克拉通中条山地区地质简图(据白瑾等,1997刘树文等, 2007)

      Fig.  2.  Geological sketch map of Zhongtiao mountains in the North China Craton (after Bai et al., 1997; Liu et al., 2007)

      图  3  横岭关二长花岗岩的野外及显微镜下照片(矿物缩写据沈其韩,2009

      a.二长花岗质片麻岩的野外特征;b.二长花岗质片麻岩的显微镜下特征,单偏光;c.绢云石英片岩的野外特征;d.绢云石英片岩的显微镜下特征,单偏光

      Fig.  3.  Field and microscopic photographs of the Henglingguan monzogranite (abbreviation of minerals after Shen, 2009)

      图  4  横岭关二长花岗岩锆石U⁃Pb年龄谐和图(a)和锆石年龄与εHf(t)关系图(b)

      球粒陨石(CHUR)根据Blichert⁃Toft and Albereade(1997); 亏损地幔(DM)根据Griffin et al.(2000); 长英质上地壳的计算根据Vervoort et al.(2000)

      Fig.  4.  U⁃Pb Concordia diagram of zircons from the Henglingguan adamellite (a) and zircon ages vs. εHf(t) (b)

      图  5  横岭关二长花岗岩SiO2-K2O(a)和A/CNK-A/NK(b)关系图解

      图a据Peccerillo and Taylor(1976)Middlemost(1985);图b中A/CNK=Al2O3/(CaO+Na2O+K2O), A/NK=Al2O3/(Na2O+K2O)

      Fig.  5.  Geochemical diagram of SiO2 vs. K2O (a) and A/CNK vs. A/NK (b) for the Henglingguan monzogranit

      图  6  横岭关二长花岗岩球粒陨石标准化稀土元素配分图(a)和原始地幔标准化微量元素蛛网图解(b)(标准化值根据Sun McDonough, 1989

      Fig.  6.  Chondrite-normalized REEs (a) and PM-normalized trace elements (b) patterns for the Henglingguan monzogranite (normalization values after Sun McDonough, 1989)

      图  7  横岭关二长花岗岩10 000 Ga/Al-TFeO/MgO(a)和SiO2-P2O5(b)判别图

      Fig.  7.  10 000 Ga/Al vs. TFeO/MgO (a) and SiO2 vs P2O5 (b) diagram of the Henglingguan monzogranite

      图  8  横岭关二长花岗岩Nb-Y(a)和Rb-(Y+Yb)(b)图解(底图据Pearce et al., 1984

      Syn⁃COLG.同碰撞花岗岩; VAG.火山弧花岗岩; WPG.板内花岗岩; ORG.洋脊花岗岩

      Fig.  8.  Nb vs. Y (a) and Rb vs. (Y+Yb) (b) diagrams of the Henglingguan monzogranite (after Pearce et al., 1984)

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