浙赣三山地区早-中奥陶世斑脱岩SHRIMP锆石U-Pb精确定年

浙赣三山地区早-中奥陶世斑脱岩SHRIMP锆石U-Pb精确定年

论文摘要

目前浙赣三山地区"金钉子"尚无精确的同位素年龄数据.基于钾质斑脱岩SHRIMP锆石U-Pb测试,三山地区早-中奥陶世宁国组Azygograptus suecicus带中部、Exigraptus clavus带底部、Acrograptus ellesae带中部的同位素年龄分别为482.9±6.1 Ma、477.6±8.3 Ma和467.0±4.4 Ma,为华南地区中奥陶世大坪阶和达瑞威尔阶底界的全球界线层型(GSSP)开展地层对比提供了精确的同位素年代学依据.结合生物带对比,大致将浙西地区早-中奥陶世普遍存在的地层缺失事件的发生时限界定于482.9~477.6 Ma之间,即杭州-嘉兴台地缺失牙形刺Oepikodus evae带-Lenodus anticariabilis带(或笔石Azygograptus suecicus带-Acrograptus ellesae带)地层,其代表了郁南运动在浙西地区的具体表现,拉开了华南地区早古生代构造运动的序幕,也可能是欧洲加里东造山过程中亨伯运动和塔康运动的远程响应.

论文目录

  • 1 地质背景
  • 2 样品采集与测试方法
  • 3 样品测试结果
  •   3.1 钾质斑脱岩地球化学特征
  •   3.2 SHRIMP锆石U-Pb定年
  •     3.2.1 三山地区宁国组A zygograptus suecicus带和Exigraptus clavus带斑脱岩锆石年龄
  •     3.2.2 三山地区宁国组Acrograptus ellesae带斑脱岩锆石年龄
  • 4 讨论
  •   4.1 对中奥陶世大坪阶和达瑞威尔阶底界的年龄限定
  •   4.2 对华南早、中奥陶世构造运动的约束
  • 5 结论
  • 文章来源

    类型: 期刊论文

    作者: 唐增才,刘风龙,董学发,余盛强,赵旭东,胡开明,陈忠大,吴小勇

    关键词: 年代学,地球化学,斑脱岩,奥陶纪,区域构造运动,三山地区

    来源: 地球科学 2019年09期

    年度: 2019

    分类: 基础科学

    专业: 地质学

    单位: 浙江省地质调查院,中国地质大学地球科学学院

    基金: 中国地质调查局地质调查项目(Nos.1212011120834,12120114068901),浙江省国土资源厅项目(Nos.2014004,2010001)

    分类号: P597.3

    页码: 2963-2977

    总页数: 15

    文件大小: 2282K

    下载量: 113

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