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    云开地块晚二叠世富Fe-Ti-P超镁铁质岩的年代学、地球化学与岩石成因

    周岱 柯贤忠 王祥东 王磊 王晶

    周岱, 柯贤忠, 王祥东, 王磊, 王晶, 2021. 云开地块晚二叠世富Fe-Ti-P超镁铁质岩的年代学、地球化学与岩石成因. 地球科学, 46(4): 1295-1310. doi: 10.3799/dqkx.2020.275
    引用本文: 周岱, 柯贤忠, 王祥东, 王磊, 王晶, 2021. 云开地块晚二叠世富Fe-Ti-P超镁铁质岩的年代学、地球化学与岩石成因. 地球科学, 46(4): 1295-1310. doi: 10.3799/dqkx.2020.275
    Zhou Dai, Ke Xianzhong, Wang Xiangdong, Wang Lei, Wang Jing, 2021. Geochronology, Geochemistry and Petrogenesis of Late Permian Fe-Ti-P-Rich Ultramafic Rocks in Yunkai Terrane, South China. Earth Science, 46(4): 1295-1310. doi: 10.3799/dqkx.2020.275
    Citation: Zhou Dai, Ke Xianzhong, Wang Xiangdong, Wang Lei, Wang Jing, 2021. Geochronology, Geochemistry and Petrogenesis of Late Permian Fe-Ti-P-Rich Ultramafic Rocks in Yunkai Terrane, South China. Earth Science, 46(4): 1295-1310. doi: 10.3799/dqkx.2020.275

    云开地块晚二叠世富Fe-Ti-P超镁铁质岩的年代学、地球化学与岩石成因

    doi: 10.3799/dqkx.2020.275
    基金项目: 

    中国地质调查局地质调查项目 12120114039201

    中国地质调查局地质调查项目 DD20160035

    中国地质调查局地质调查项目 DD20190047

    中国地质调查局地质调查项目 DD20211385

    详细信息
      作者简介:

      周岱(1985-), 高级工程师, 岩石学专业, 长期从事华南云开地区和海南岛区域地质调查和综合研究工作.ORCID: 0000-0002-2666-8848.E-mail: 281045030@qq.com

    • 中图分类号: P59;P581

    Geochronology, Geochemistry and Petrogenesis of Late Permian Fe-Ti-P-Rich Ultramafic Rocks in Yunkai Terrane, South China

    • 摘要: 为了更好地理解华南板块南缘二叠纪与三叠纪之交复杂的构造格局,通过岩石学、地球化学和年代学的方法,对粤西云开地区新发现的3处晚二叠世超镁铁质侵入岩进行了研究.这些岩石位于云开地块东缘的阳春三甲和地块中部的高州大井、东岸等地,呈小岩株、岩脉产出于云开岩群的片岩、变粒岩中.它们的主要岩性为辉石岩、角闪石岩、角闪岩和斜长角闪岩,锆石SHRIMP和LA-ICP-MS U-Pb定年获得的岩石形成时代为253~259 Ma.超镁铁质侵入岩富(含钛)磁铁矿、榍石和磷灰石,显示出显著富集Fe-Ti-P的地球化学特征,并表现为轻稀土中等富集,微量元素亏损Nb-Ta-Zr-Hf的特征.全岩εNdt)集中在-3.4~-10.0之间,锆石εHft)介于-1.2~-9.5,锆石δ18O集中于7.01‰~9.71‰,表现为富集岩石圈地幔源区特征.研究认为,二叠纪峨眉山地幔柱活动(~259 Ma)的影响范围可能波及到了粤桂交界的云开地区,地幔柱热流导致岩石圈地幔部分熔融形成玄武质岩浆,经不同程度的结晶分异作用,最终形成了云开晚二叠世富Fe-Ti-P超镁铁质岩.

       

    • 图  1  华南板块二叠纪-三叠纪构造格局与主要岩浆岩分布

      Faure et al.(2016)修改

      Fig.  1.  Structural framework and igneous rocks of South China block in the Permian-Triassic

      图  2  云开地块地质简图(a)、阳春三甲超镁铁质侵入体地质图(b)和大井-东岸地区地质简图(c)

      Fig.  2.  Geological map of Yunkai terrane(a) and ultramafic intrusion maps (b, c)

      图  3  典型野外露头及岩石镜下特征

      a.大井上平废弃采石场外貌;b.角闪石岩,角闪石粒径粗大,集中在3~15 mm;c.东岸上垌超镁铁质岩露头不佳,所见多为风化壳内的准原地滚石;d~e.三甲(磷灰石磁铁矿)角闪石岩,含钛磁铁矿呈海绵陨铁状-浸染状填充在角闪石晶间,呈堆晶结构;f.三甲黑云母辉石岩;g~h.大井上平角闪岩,粗大的角闪石晶内及晶间包裹大量细小的磷灰石、榍石和含钛磁铁矿;i.东岸上平石榴斜长角闪岩.图 3e为正交平光,其他为单偏光.Hbl.角闪石;Mag.磁铁矿;Ap.磷灰石;Ttn.榍石;Grt.石榴石;Pl.斜长石;Cpx.单斜辉石;Bt.黑云母

      Fig.  3.  Field and microscopic photos of typical ultramafic rocks

      图  4  变基性岩原岩判别(a)和TAS图解(b)

      图a据Misra(1971); 图b据Middlemost(1994),矾山数据引自Hou et al.(2015)

      Fig.  4.  Identification of the origin of metabasites (a) and TAS classification diagram(b) of the ultramafic rocks

      图  5  超镁铁质岩Mg#与主量元素、Ni、Zr元素和(La/Yb)n比值哈克图解

      Fig.  5.  Major elements and Ni, Zr covariation diagrams of the ultramafic rocks

      图  6  超镁铁质岩全岩Fe-Ti含量变化特征

      Fig.  6.  FeOT vs. TiO2 and Fe2O3 vs. TiO2 covariation diagrams of the ultramafic rocks

      图  7  球粒陨石标准化稀土元素配分模式图解(a, c)和原始地幔标准化微量元素蛛网图解(b, d)

      Fig.  7.  Chondrite-normalized REE patterns(a, c) and primitive-mantle normalized multi-elemental spider diagrams(b, d) of ultramafic rocks

      图  8  超镁铁质岩SiO2Nd(t)(a)和ISrNd(t)(b)图解

      峨眉山玄武岩和矾山数据分别引自Luo et al.(2014)Hou et al.(2015)

      Fig.  8.  SiO2Nd(t) (a) and ISrNd(t) (b) diagrams of ultramafic rocks

      图  9  超镁铁质岩锆石阴极发光图像

      数字为206Pb/238U表面年龄和δ18O值

      Fig.  9.  Photomicrographs of all zircons analyzed for U-Pb ages and O isotopes

      图  10  超镁铁质岩锆石U-Pb谐和图

      Fig.  10.  U-Pb concordia plots of ultramafic rocks

      图  11  东岸上垌石榴斜长角闪岩(15SD25-1)锆石Th-U与稀土元素特征

      Fig.  11.  Th vs. U and chondrite-normalized REE patterns of zircons of plagioclase amphibolite(15SD25-1) from Dong'an Shangdong

      图  12  大井上平角闪岩(15DJ13)锆石Hf-O同位素组成

      竹雅、石板辉长岩数据周岱等(2017);龙虎岗辉绿岩数据引自Wang et al.(2013)

      Fig.  12.  Zircon Hf-O isotopic element of amphibolite (15DJ13) from Dajing Shangping

      图  13  超镁铁质岩Th/Yb-Nb/Yb图解(a)和TiO2/Yb-Nb/Yb图解(b)

      底图据Pearce(2008);云开早古生代基性岩据Wang et al.(2013)周岱等(2017)

      Fig.  13.  Discrimination diagrams of Th/Yb vs. Nb/Y (a) and TiO2/Yb vs. Nb/Yb (b) for the ultramafic rocks

      表  1  云开地块及周边地区二叠纪至三叠纪典型岩浆岩统计

      Table  1.   The typical igneous rocks in Yunkai terrane and adjacent area between Permian and Triassic

      分布区域 岩体名称 主要岩性 形成年龄(Ma) 数据来源
      桂东南 大容山-六万大山-十万大山 堇青石黑云母花岗岩、石榴石紫苏辉石花岗岩 248~251 Jiao et al., 2015王磊等,2016
      桂东南 那丽 堇青石黑云母二长花岗岩 262~265 贾小辉等,2012Li et al., 2016
      粤西 阳春三甲、高州上平-上垌 辉石岩、角闪石岩 253~259 本文
      粤西 岑溪安平 辉长岩、辉绿岩 248~252 Xu et al., 2018
      粤西 新兴 黑云母二长花岗岩 240~224 未发表数据
      粤西 那蓬 混合花岗岩 245~231 柯贤忠等,2018
      川滇、黔、桂西 峨眉山大火成岩省 玄武岩、辉长岩、辉绿岩 259 Zhong et al., 2014Fan et al., 2008
      海南 五指山、尖峰岭、黎母岭 花岗岩、碱性岩、辉长岩 280~220 谢才富等,2006Li et al., 2006
      下载: 导出CSV
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