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现代地质 ›› 2020, Vol. 34 ›› Issue (05): 1028-1042.DOI: 10.19657/j.geoscience.1000-8527.2020.042

• 岩石学 • 上一篇    下一篇

贵州官坝地区二叠系—三叠系地质界面黏土岩的火山岩特征、LA-ICP-MS 锆石U-Pb年龄及其地质意义

何碧1(), 张向文1, 赵飞1, 金灿海2, 任光明2, 王宁祖1, 张文斌1, 张志玺1, 孙平原1   

  1. 1.甘肃省地质矿产勘查开发局 第二地质矿产勘查院,甘肃 兰州 730020
    2.中国地质调查局 成都地质调查中心,四川 成都 610081
  • 收稿日期:2018-09-12 修回日期:2020-06-16 出版日期:2020-10-28 发布日期:2020-10-29
  • 作者简介:何 碧,男,硕士,工程师,1990年出生,古生物学与地层学专业,主要从事区域地质与生态环境地质工作。Email: hebidzxgsw@163.com
  • 基金资助:
    中国地质调查局地质调查项目“乌蒙山区地质矿产综合调查”项目(DD20160019);中国地质调查局成都地质调查中心项目“贵州乌蒙山区1∶5万店子场(G48E006018)、大关(G48E007017)、六厂(G48E0070183)幅区域地质调查”(DD20160019-04)

Volcanic Characteristics, LA-ICP-MS Zircon U-Pb Ages of Claystone at the Permian-Triassic Boundary, Guanba Area in Guizhou Province, South China and the Geological Implications

HE Bi1(), ZHANG Xiangwen1, ZHAO Fei1, JIN Canhai2, REN Guangming2, WANG Ningzu1, ZHANG Wenbin1, ZHANG Zhixi1, SUN Pingyuan1   

  1. 1. The Second Institute of Geology and Minerals Exploration Team,Gansu Provincial Bureau of Geology and Minerals Exploration and Development,Lanzhou,Gansu 730020,China
    2. Chengdu Center,China Geological Survey,Chengdu,Sichuan 610081,China
  • Received:2018-09-12 Revised:2020-06-16 Online:2020-10-28 Published:2020-10-29

摘要:

贵州省黔西县官坝地区位于华南板块西南部,其二叠系—三叠系界线剖面出露较好,界线处出露3层黏土岩。采集贵州黔西官坝地区二叠系—三叠系地质界面黏土岩1件U-Pb年龄样品、7件地球化学样品,对其锆石进行U-Pb定年以及主量、微量和稀土元素进行测试分析。锆石 LA-ICP-MS U-Pb分析结果表明,U和Th含量分别为60.26×10 -6~297.9×10 -6和46.14×10 -6~244.26×10 -6,Th/U比值介于0.76~1.55之间,为典型的岩浆锆石;获得 206Pb/ 238U加权平均年龄为(252.6±1.4) Ma,谐和年龄为(252.7±0.6) Ma。地球化学分析结果显示,黏土岩属于高硅、铝、钾、镁,低铁、钛的钙碱质中酸性火山物质,具有稀土元素总量相对较高、相对富集轻稀土元素和轻、重稀土元素分馏程度高的特征,负Eu异常明显,δEu =0.19~0.45。上述岩石地球化学特征表明,贵州黔西官坝地区(华南板块西南)二叠系—三叠系界线位置总体上可与浙江长兴(华南板块东南)海相二叠系—三叠系界线(金钉子)相比较。

关键词: 二叠系—三叠系界线;, 黏土岩, LA-ICP-MS锆石 U-Pb年龄, 官坝地区

Abstract:

Three Permian-Triassic claystone are outcropped at Guanba (Qianxi County) in Guizhou Province, geologically in the southwestern South China block. One sample for zircon U-Pb dating and 7 samples for geochemical analysis were collected from the base of the claystone. LA-ICP-MS zircon U-Pb analysis shows that the zircons have 60.26×10 -6-297.90×10 -6 U and 46.14×10 -6-244.26×10 -6 Th, with Th/U value of 0.76-1.55, resembling typical igneous zircons. Zircon U-Pb dating yielded a 206Pb/ 238U weighted mean age of (252.6±1.4) Ma, and the concordant age of (252.7±0.6) Ma. Geochemical analysis shows that the tuff contains calc-alkaline volcanic materials with high Si-Al-K-Mg contents and low Fe-Ti contents. Additionally, the claystone has relatively high total REE contents, with elevated LREE enrichments and REE fractionation. Negative Eu anomaly is obvious (δEu=0.19-0.45). Geochemical characteristics indicate that the Permian-Triassic boundary at Guanba is comparable to the marine-facies Permian-Triassic boundary at Changhsing (GSSP, southeastern South China block).

Key words: Permian-Triassic boundary, claystone, LA-ICP-MS zircon U-Pb dating, Guanba area, Guizhou Province

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