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    吉林通化赤柏松地区早白垩世花岗质岩脉(株)的成因:锆石U-Pb年代学、Hf同位素和地球化学证据

    周皓 裴福萍 焦骥 王枫 许文良

    周皓, 裴福萍, 焦骥, 王枫, 许文良, 2020. 吉林通化赤柏松地区早白垩世花岗质岩脉(株)的成因:锆石U-Pb年代学、Hf同位素和地球化学证据. 地球科学, 45(2): 519-533. doi: 10.3799/dqkx.2018.309
    引用本文: 周皓, 裴福萍, 焦骥, 王枫, 许文良, 2020. 吉林通化赤柏松地区早白垩世花岗质岩脉(株)的成因:锆石U-Pb年代学、Hf同位素和地球化学证据. 地球科学, 45(2): 519-533. doi: 10.3799/dqkx.2018.309
    Zhou Hao, Pei Fuping, Jiao Ji, Wang Feng, Xu Wenliang, 2020. Petrogenesis of Early Cretaceous Chibaisong Granitoid Dyke (Stock) from Tonghua Area, Jilin Province: Evidences from Zircon U-Pb Geochronology, Hf Isotope and Whole-Rock Geochemistry. Earth Science, 45(2): 519-533. doi: 10.3799/dqkx.2018.309
    Citation: Zhou Hao, Pei Fuping, Jiao Ji, Wang Feng, Xu Wenliang, 2020. Petrogenesis of Early Cretaceous Chibaisong Granitoid Dyke (Stock) from Tonghua Area, Jilin Province: Evidences from Zircon U-Pb Geochronology, Hf Isotope and Whole-Rock Geochemistry. Earth Science, 45(2): 519-533. doi: 10.3799/dqkx.2018.309

    吉林通化赤柏松地区早白垩世花岗质岩脉(株)的成因:锆石U-Pb年代学、Hf同位素和地球化学证据

    doi: 10.3799/dqkx.2018.309
    基金项目: 

    国家重点研发计划项目 2016YFC0600108-02

    吉林大学研究生创新研究计划 101832018C037

    详细信息
      作者简介:

      周皓(1993-), 男, 硕士, 主要从事火成岩岩石学研究

      通讯作者:

      裴福萍

    • 中图分类号: P581

    Petrogenesis of Early Cretaceous Chibaisong Granitoid Dyke (Stock) from Tonghua Area, Jilin Province: Evidences from Zircon U-Pb Geochronology, Hf Isotope and Whole-Rock Geochemistry

    • 摘要: 中国吉林省通化县赤柏松地区早白垩世花岗质岩脉(株)的锆石U-Pb年代学、Hf同位素和全岩地球化学特征,为探讨华北克拉通东北部中生代时期大陆下地壳的属性和构造演化历史提供了重要依据.研究区花岗质岩脉(株)中的锆石普遍发育振荡生长环带,并具有较高的Th/U比值(0.53~1.94),表明其为岩浆成因.对采自花岗质岩脉(株)中4个样品的锆石U-Pb测年结果表明,它们的206Pb/238U加权平均年龄分别为116 Ma、124 Ma、127 Ma和130 Ma,即早白垩世早期和早白垩世晚期.这些花岗质岩石具有变化的SiO2(60.61%~76.07%)和MgO(0.01%~2.48%)含量、富碱(K2O+Na2O=6.26%~9.14%)及富Al2O3(11.99%~16.13%)的特征,总体属于高钾钙碱性系列岩石.微量元素上富集轻稀土和大离子亲石元素,亏损重稀土和Ba、Sr、P、Ti和Eu等元素(Eu/Eu*=0.05~0.30),暗示其主要来自地壳岩石的部分熔融,并在演化过程中经历了斜长石、碱性长石、磷灰石和钛铁矿等矿物的分离结晶作用和围岩的同化混染作用.与早白垩世早期花岗质岩石相比,早白垩世晚期岩石的碱性程度提高.样品中锆石εHft)值介于-21.84~-10.74之间,两阶段亏损地幔模式年龄为1.86~2.56 Ga.上述地球化学特征暗示,赤柏松地区下地壳以古元古代地壳物质为主,存在少量新太古代地壳物质.早白垩世时期研究区以双峰式岩石组合为特征,进一步结合区域上已有的火成岩和区域构造演化的研究成果,认为早白垩世时期研究区处于俯冲背景下的伸展环境.与早白垩世早期相比,早白垩世晚期伸展作用增强.

       

    • 图  1  华北克拉通构造简图(a)和通化赤柏松地区地质简图(b)

      Fig.  1.  Simplified geological maps showing (a) major tectonic units of North China Craton and (b) of the Chibaisong area in Tonghua

      图  2  通化赤柏松地区早白垩世花岗质岩石镜下照片

      Qz.石英; Or.正长石; Pl.斜长石; a.花岗斑岩;b.花岗斑岩;c.石英的熔蚀结构、斜长石的碳酸盐化;d.环斑球粒结构

      Fig.  2.  Photomicrographs showing the petrographic features of Early Cretaceous granitoids of the Chibaisong area in Tonghua

      图  3  通化赤柏松地区早白垩世花岗质岩石中部分锆石的阴极发光图像

      红色实线圆圈为U-Pb年龄测试点; 黄色虚线圆圈为Hf同位素测试点; 括号内为Hf同位素测试值; 左侧短线为比例尺100 μm

      Fig.  3.  Cathodoluminescence (CL) images of selected zircon grains of Early Cretaceous granitoids of the Chibaisong area in Tonghua

      图  4  通化赤柏松地区早白垩世花岗质岩石锆石LA-ICP-MS U-Pb年龄谐和图

      Fig.  4.  LA-ICP-MS zircon U-Pb concordia diagrams for Early Cretaceous granitoids in the Chibaisong area, Tonghua.

      图  5  (a)通化赤柏松地区早白垩世花岗质岩石SiO2 vs. (Na2O+K2O)图解; (b)SiO2vs.K2O图解

      Peccerillo and Taylor(1976)Middlemost(1994);数据裴福萍等(2009), Pei et al.(2011a), 杨凤超等,(2017), 秦亚等(2013)

      Fig.  5.  Plots of SiO2 vs. (Na2O+K2O) (a), SiO2 vs K2O (b) for the Early Cretaceous granitoids in the Chibaisong area, Tonghua

      图  6  通化赤柏松地区早白垩世花岗质岩石球粒陨石标准化稀土元素配分型式(a)和原始地幔标准化微量元素蛛网图(b)

      球粒陨石标准数据Preston et al.(1985); 原始地幔标准化数据Sun and McDonough (1984); 图例同图 5

      Fig.  6.  (a) Chondrite-normalized REE patterns and (b) primitive mantle (PM)-normalized trace element spider diagrams for the Early Cretaceous granitoids in the Chibaisong area, Tonghua

      图  7  通化赤柏松地区早白垩世花岗质岩石的Hf同位素组成

      Yang et al.(2006);CAOB.中亚造山带;YFTB.燕山褶皱带;数据杨凤超等(2017)Zhang et al.(2018)

      Fig.  7.  Correlations between Hf isotopic compositions and ages of zircons for the Early Cretaceous granitoids in the Chibaisong area, Tonghua

      图  8  通化赤柏松地区早白垩世花岗质岩石Ba-Sr和Rb/Sr-Sr图解(图例同图 5

      Fig.  8.  Ba-Sr and Rb/Sr-Sr diagram for the Early Cretaceous granitoids in the Chibaisong area, Tonghua

      图  9  通化赤柏松地区早白垩世花岗质岩石的成因类型判别图解(a)Zr+Nb+Ce+Y-(Na2O+K2O)/CaO;(b)Zr+Nb+Ce+Y-FeO*/MgO(据Whalen et al., 1987

      Fig.  9.  (a) (Na2O+K2O)/CaO vs. (Zr+Nb+Ce+Y) and (b) FeO*/MgO vs. (Zr+Nb+Ce+Y) discrimination diagrams

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