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    丽江盆地早三叠世砂岩物源特征及其对扬子西南构造的约束

    朱民 孟立丰 李也 陈新伟 吴鸿翔

    朱民, 孟立丰, 李也, 陈新伟, 吴鸿翔, 2025. 丽江盆地早三叠世砂岩物源特征及其对扬子西南构造的约束. 地球科学, 50(11): 4424-4441. doi: 10.3799/dqkx.2025.138
    引用本文: 朱民, 孟立丰, 李也, 陈新伟, 吴鸿翔, 2025. 丽江盆地早三叠世砂岩物源特征及其对扬子西南构造的约束. 地球科学, 50(11): 4424-4441. doi: 10.3799/dqkx.2025.138
    Zhu Min, Meng Lifeng, Li Ye, Chen Xinwei, Wu Hongxiang, 2025. Provenance of Early Triassic Clastic Rocks and Its Constraint on Tectonic Evolution of Lijiang Basin, Upper Yangtze Block. Earth Science, 50(11): 4424-4441. doi: 10.3799/dqkx.2025.138
    Citation: Zhu Min, Meng Lifeng, Li Ye, Chen Xinwei, Wu Hongxiang, 2025. Provenance of Early Triassic Clastic Rocks and Its Constraint on Tectonic Evolution of Lijiang Basin, Upper Yangtze Block. Earth Science, 50(11): 4424-4441. doi: 10.3799/dqkx.2025.138

    丽江盆地早三叠世砂岩物源特征及其对扬子西南构造的约束

    doi: 10.3799/dqkx.2025.138
    基金项目: 

    国家自然科学基金项目 42062014

    江西省教育厅科学技术研究项目 A00129

    详细信息
      作者简介:

      朱民(1984-),男,副教授,博士,主要从事沉积学、造山带和盆地构造分析.ORCID:0000-0002-8002-2159. E-mail:237623510@qq.com

      通讯作者:

      孟立丰,E-mail:lifengmeng@zjut.edu.cn

    • 中图分类号: P531

    Provenance of Early Triassic Clastic Rocks and Its Constraint on Tectonic Evolution of Lijiang Basin, Upper Yangtze Block

    • 摘要: 丽江盆地作为扬子西南边缘地区多板块交汇带,对其下三叠统沉积物源的研究可掲示扬子西南地区的沉积“源‒汇系统”及其与西部冈瓦纳弧盆体系的时空关系.野外观测与镜下鉴定显示鹤庆腊美组砂岩均来自近距离的长英质火山岩物质,且碎屑锆石分别呈现~254 Ma和~255 Ma单一年龄峰值,与峨眉山大火成岩省中酸性岩浆活动时间一致,与板内/非造山环境岩浆锆石具有锆石微量元素一致性,而区别于弧造山带;Lu-Hf同位素εHft)值表明其与峨眉山大火成岩省的长英质岩类有关系;全岩地球化学数据显示腊美组与峨眉山流纹岩、粗面岩、正长岩具有主微量元素一致的特征.综合分析得腊美组物源来自近源搬运的峨眉山流纹岩、粗面岩和正长岩.早三叠世期间丽江盆地仍为被动陆缘沉积,主要接受来自峨眉山大火成岩省的物质,无西部弧盆体系物质来源.

       

    • 图  1  丽江盆地及邻区地质简图

      a,b. 据云南省地质局(1966);c.据Munteanu et al.(2013)修改;d.据Metcalfe(2013)修改

      Fig.  1.  Simplified geologic map of the Lijiang basin and its adjacent areas

      图  2  丽江地区早三叠世腊美组野外实测剖面(a, b)(剖面位置见图a, b)

      Fig.  2.  Stratigraphic columns (a, b) of the Early Triassic Lamei Formation in Lijiang area

      图  3  吉地坪和后本菁剖面早三叠世腊美组样品野外(a, d)及镜下(b, c, e, f)正交偏光特征

      黄实线为层理,黄虚线为交错层理. Q. 石英;Kfs. 钾长石;Lvf. 长英质火山岩屑;Lvm. 微晶火山岩屑;Lvl. 板条状火山岩屑;Pl. 斜长石

      Fig.  3.  Field work of the Early Triassic Lamei Formation in Jidiping (a), Houbenjing (d) and their micro photographs (b, c, e, f) for sandstone samples

      图  4  丽江吉地坪剖面(a)和后本菁剖面(b)下三叠统样品典型锆石颗粒阴极发光照片

      红圈代表年龄,黄圈代表Hf点位

      Fig.  4.  LA-ICP-MS zircon U-Pb representative cathode-luminescence (CL) from samples of the Lower Triassic in Jidiping (a) and Houbenjing (b) areas

      图  5  丽江吉地坪(a, b)和后本菁(c, d)地区剖面早三叠世砂岩碎屑锆石U-Pb年龄频谱及协和图

      Fig.  5.  U-Pb concordia and histogram diagrams of Jidiping (a, b) and Houbenjing (c, d) detrital zircons

      图  6  腊美组稀土元素CL球粒陨石配分模式(a, b)和微量元素Hf/Th-Th/Nb(c, d)判别图解

      球粒陨石稀土元素含量参照Sun and Mc Donough(1989);微量元素判别图据Yang et al.(2012),峨眉山流纹岩数据据Xu et al.(2008)Shellnutt et al.(2009)Hei et al.(2018)

      Fig.  6.  The CL chondrite-normalized rare earth element diagrams (a, b) and Hf/Th-Th/Nb discriminating (c, d) for the detrital zircons of the Lamei sandstones

      图  7  吉地坪和后本菁剖面腊美组碎屑锆石εHf(t)值与U-Pb年龄的关系

      峨眉山流纹岩数据据Xu et al.(2010)Hei et al.(2018)Huang et al.(2022a);峨眉山玄武岩数据据Xu et al.(20012008)Xiao et al.(2004)Shellnutt et al.(2009)Zhong et al.(2009);峨眉山正长岩数据据Xu et al.(2008)Shellnutt et al.(2009);泛大洋弧岩浆岩(He et al.,2018Shen et al.,2018Wang et al.,2021)+华南PTB火山岩数据(高秋灵,2013He et al.,2014王曼等,2018Wang et al.,2019)以及江达维西弧长英质火山岩数据(Wang et al.,2014

      Fig.  7.  Plot of zircon εHf (t) versus 206Pb/238U age (Ma) for the Lamei Formation in Jidiping and Houbenjing areas

      图  8  腊美组样品微量元素蛛网(a, b)和稀土元素球粒陨石标准化配分模式(c, d)

      球粒陨石和原始地幔标准化数据引自Sun and McDonough(1989),UCC标准数据引自Taylor and McLennan(1985)

      Fig.  8.  The spider web of trace elements (a, b) and the standardized distribution model diagram of rare earth element chondrites (c, d) of the Lamei Formation samples

      图  9  腊美组细碎屑岩全岩主量元素A-CN-K(a)及微量元素Th/U-Th比值(b)

      Fig.  9.  Geochemical relations of A-CN-K (a) and Th/U-Th (b) for the samples from Lamei Formation

      图  10  鹤庆下三叠统腊美组砂岩物源构造背景判别图解

      a.Q-F-L;b. Qm-F-Lt(Dickinson et al.,1983;部分数据高崇龙等,2024). V.火山岩组分;P.深成岩组分

      Fig.  10.  Modal composition triangle diagrams for the samples from Lamei Formation in the Lower Triassic from Heqing

      图  11  丽江盆地鹤庆吉地坪(c)、后本菁腊美组(b)(本文)与大理邓川青天堡组(d,e)、上沧下三叠统砾岩(韩超,2023) (f)以及已报道华南地区(a)下三叠统(张英利等,2016Zhu et al., 2018缪宇等,2021Meng et al., 2022周寅生等,2022邓旭升等,2025)和EILP(g)碎屑锆石年龄谱对比图

      Fig.  11.  Probability density plots and histograms of detrital zircon U-Pb ages for the Lamei Formation from the Heqing Jidiping (c) and Houbenjing (b), Qingtianbao Formation from Dengchuan (d, e), the Lower Triassic from Shangcang (f), EILP(g) and South China block (a, published)

      图  12  腊美组砂岩K2O/Na2O-SiO2 (a)、Th/Sc-Zr/Sc (b)、Co/Th-La/Sc (c)和Ti-Zr (d)比值

      UCC数据引自Taylor and McLennan(1985),峨眉山正长岩+粗面岩数据自Xu et al.(2008)Shellnutt et al.(2009)Zhong et al.(2009);峨眉山流纹岩数据据Xu et al.(2010)Cheng et al.(2017)Hei et al.(2018)Huang et al.(2022a)

      Fig.  12.  Ratio of K2O/Na2O-SiO2 (a), Th/Sc-Zr/Sc (b), Co/Th-La/Sc (c) and Ti-Zr (d) in sandstone of Lamei Formation

      图  13  早三叠世丽江盆地岩相古地理(a)和构造演化(b~d)

      四川省地质矿产研究所专题研究组(1987)崔克信(2004)马永生等(2009)

      Fig.  13.  The lithofacies and paleogeographic sketch (a) and the tectonic evolution (b‒d) of Lijiang area in Early Triassic

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    • 收稿日期:  2025-04-21
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