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
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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