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    越南昆嵩地体三叠纪花岗岩岩石成因及其特提斯构造意义

    李慧玲 钱鑫 余小清 PhamTrungHieu 张菲菲 余永琪 徐畅 王岳军

    李慧玲, 钱鑫, 余小清, PhamTrungHieu, 张菲菲, 余永琪, 徐畅, 王岳军, 2023. 越南昆嵩地体三叠纪花岗岩岩石成因及其特提斯构造意义. 地球科学, 48(4): 1441-1460. doi: 10.3799/dqkx.2022.335
    引用本文: 李慧玲, 钱鑫, 余小清, PhamTrungHieu, 张菲菲, 余永琪, 徐畅, 王岳军, 2023. 越南昆嵩地体三叠纪花岗岩岩石成因及其特提斯构造意义. 地球科学, 48(4): 1441-1460. doi: 10.3799/dqkx.2022.335
    Li Huiling, Qian Xin, Yu Xiaoqing, Pham Trung Hieu, Zhang Feifei, Yu Yongqi, Xu Chang, Wang Yuejun, 2023. Petrogenesis of Triassic Granites from Kontum Massif in Vietnam and Its Tethyan Tectonic Implications. Earth Science, 48(4): 1441-1460. doi: 10.3799/dqkx.2022.335
    Citation: Li Huiling, Qian Xin, Yu Xiaoqing, Pham Trung Hieu, Zhang Feifei, Yu Yongqi, Xu Chang, Wang Yuejun, 2023. Petrogenesis of Triassic Granites from Kontum Massif in Vietnam and Its Tethyan Tectonic Implications. Earth Science, 48(4): 1441-1460. doi: 10.3799/dqkx.2022.335

    越南昆嵩地体三叠纪花岗岩岩石成因及其特提斯构造意义

    doi: 10.3799/dqkx.2022.335
    基金项目: 

    国家自然科学基金项目 41830211

    国家自然科学基金项目 42072256

    广东省基础与应用基础研究基金项目 2018B030312007

    广东省基础与应用基础研究基金项目 2019B1515120019

    中山大学高校基本业务费 22lgqb14

    详细信息
      作者简介:

      李慧玲(1998-), 女, 硕士研究生, 地球化学专业.ORCID: 0000-0002-3590-1197.E-mail: lihling33@mail2.sysu.edu.cn

      通讯作者:

      钱鑫, ORCID: 0000-0002-3587-861X.E-mail: qianx3@mail.sysu.edu.cn

    • 中图分类号: P597

    Petrogenesis of Triassic Granites from Kontum Massif in Vietnam and Its Tethyan Tectonic Implications

    • 摘要: 昆嵩地体位于印支陆块的核部,记录了大量的印支期岩浆作用和构造热事件,是了解古特提斯洋演化及印支与华南陆块碰撞拼合过程的关键区域,但目前对该期岩浆事件的成因及其与北部长山带的关系未能得到有效厘定.对昆嵩地体绥安(Huyện Tuy An)和胶寮(Chu Loan)地区的Van Canh花岗岩开展了岩相学、锆石U-Pb年代学、锆石原位Hf同位素和全岩地球化学分析,以限定其形成时代、岩石成因及构造环境.锆石U-Pb定年显示花岗岩样品的结晶年龄为244~239 Ma.该套样品包括了二长花岗岩和钾长花岗岩,均属于高钾钙碱性系列.它们的A/CNK值为1.03~1.21,为S型花岗岩.花岗岩均显示明显的Rb、Th和U富集,以及Nb、Sr、Zr和Ti的亏损,并具有强烈的Eu负异常(Eu/Eu*=0.24~0.56).锆石具有富集的原位Hf同位素组成(εHft)=-11.2~-0.7)以及古-中元古代的Hf二阶模式年龄(TDM2=1.98~1.31 Ga).研究表明该套中三叠世花岗岩是古元古代-中元古代变沉积岩部分熔融的产物,并伴有少量变火成岩的加入.研究结合区域地质资料表明昆嵩地体中三叠世Van Canh花岗岩的成因与马江古特提斯分支洋闭合之后的印支与华南陆块的碰撞拼合有关,形成于后碰撞阶段,进而证实了长山带向南可以延伸至昆嵩地体内部.

       

    • 图  1  东南亚地区构造划分简图(a)和研究区地质简图及长山带和昆嵩地体二叠纪-三叠纪岩浆岩与变质岩年龄分布(b)

      图a据Sone and Metcalfe(2008)Wang et al.(2018)Qian et al.(2020);图b年龄数据据来源:[1] Shi et al.(2015);[2] Hieu et al.(2015);[3] Nakano et al.(2013);[4] Nagy et al.(2001);[5] Carter et al.(2001);[6] Hung et al.(2022);[7] Cuong et al.(2021)

      Fig.  1.  Tectonic sketch map of SE Asia (a) and simplified geological map of the study area and the distribution of the Permian-Triassic felsic and metamorphic rocks in the Truong Son zone and Kontum massif (b)

      图  2  昆嵩地体南部三叠纪Van Canh花岗岩野外露头和显微岩相学特征

      a~f.二长花岗岩(20VN-23,20VN-24和20VN-25);g,h.钾长花岗岩(20VN-29). 矿物缩写:Q.石英;Pl.斜长石;Kfs.钾长石;Bt.黑云母;Ms.白云母;Ep.绿帘石;Lpd.锂云母

      Fig.  2.  Field photos and photomicrographs of the Triassic Van Canh granites in southern Kontum massif

      图  3  昆嵩地体南部三叠纪Van Canh花岗岩锆石CL图像

      Fig.  3.  Cathodoluminescence (CL) images of the representative zircon grains for the Triassic Van Canh granites in southern Kontum massif

      图  4  昆嵩地体南部三叠纪Van Canh花岗岩锆石U-Pb年龄协和图

      Fig.  4.  Zircon U-Pb concordia diagrams for the Triassic Van Canh granites in southern Kontum massif

      图  5  昆嵩地体南部三叠纪Van Canh花岗岩锆石εHf (t)-年龄(Ma)图解

      背景数据引自Hieu et al.(2015)Wang et al.(2018)Hung et al.(2022)

      Fig.  5.  Plot of εHf (t) vs. age (Ma) for zircon grains from the Triassic Van Canh granites in southern Kontum massif

      图  6  昆嵩地体南部三叠纪Van Canh花岗岩

      a. An-Ab-Or判别图解;b.K2O-SiO2判别图解;c.A/NK-A/CNK判别图解;d.(Al2O3-(Na2O+K2O))-CaO-(FeOt+MgO)判别图解;e.10 000*Ga/Al-(Zr+Nb+Ce+Y)判别图解;f.(Al2O3+CaO)/(FeOt+Na2O+K2O)-100×(MgO+FeOt+TiO2)/SiO2判别图解.图a~f背景数据引自Hieu et al.(2015)Hung et al.(2022);图b据Winchester and Floyd(1977);图d据Chappell and White(1992);图e据Whalen et al.(1987);图f据Sylvester(1989)

      Fig.  6.  Triassic Van Canh granites in southern Kontum massif

      图  7  昆嵩地体南部三叠纪Van Canh花岗岩哈克图解

      背景数据引自Hieu et al.(2015)Hung et al.(2022)

      Fig.  7.  Harker diagrams for the Triassic Van Canh granites in southern Kontum massif

      图  8  昆嵩地体南部三叠纪Van Canh花岗岩球粒陨石标准化稀土元素配分曲线(a)和原始地幔标准化微量元素蛛网图(b)

      Fig.  8.  Chondrite-normalized REE patterns (a) and primitive mantle-normalized trace element spidergram (b) for the Triassic Van Canh granites in southern Kontum massif

      图  9  昆嵩地体南部三叠纪Van Canh花岗岩La/Sm-La (a)、Rb-Sr (b)和Ba-Sr (c)图解

      背景数据引自Hieu et al.(2015)Hung et al.(2022);图b和图c据Li et al.(2007)

      Fig.  9.  Plots of La/Sm vs. La (a), Rb vs. Sr (b) and Ba vs. Sr (c) for the Triassic Van Canh granites in southern Kontum massif

      图  10  昆嵩地体南部三叠纪Van Canh花岗岩3×CaO-Al2O3/(FeOt+MgO)-5×K2O/Na2O(a)和(Na2O+K2O)/(FeOt+MgO+TiO2)-(Na2O+K2O+FeOt+MgO+TiO2) (b)图解

      对比数据引自Hieu et al.(2015)Hung et al.(2022);背景数据据Laurent et al.(2014)Patiño Douce and Harris(1998)Patiño Douce(1999)

      Fig.  10.  Plots of 3×CaO vs. Al2O3/(FeOt+MgO) vs.5×K2O/Na2O (a) and (Na2O+K2O)/(FeOt+MgO+TiO2) vs. Na2O+K2O+FeOt+MgO+TiO2 (b) for the Triassic Van Canh granites in southern Kontum massif

      图  12  昆嵩地体三叠纪已发表岩浆岩和变质岩年龄汇总(年龄数据据附表4)

      Fig.  12.  Summary of the published Triassic ages for the igneous and metamorphic rocks from the Kontum massif

      图  11  昆嵩地体南部三叠纪Van Canh花岗岩构造环境判别图

      背景数据引自Hieu et al.(2015)Hung et al.(2022);图据Pearce et al.(1996)

      Fig.  11.  Tectonic discrimination diagram for the Triassic Van Canh granites in southern Kontum massif

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    出版历程
    • 收稿日期:  2022-07-12
    • 刊出日期:  2023-04-25

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