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首页|期刊导航|成都理工大学学报(自然科学版)|华北克拉通中部造山带吕梁群的形成时代与构造环境

华北克拉通中部造山带吕梁群的形成时代与构造环境

卢成森 钱加慧 尹常青 张健 高彭 吴尚京

成都理工大学学报(自然科学版)2025,Vol.52Issue(3):523-541,19.
成都理工大学学报(自然科学版)2025,Vol.52Issue(3):523-541,19.DOI:10.12474/cdlgzrkx.2024032201

华北克拉通中部造山带吕梁群的形成时代与构造环境

Formation age and tectonic setting of the Lüliang Group in the Trans-North China Orogen,North China Craton

卢成森 1钱加慧 1尹常青 1张健 2高彭 3吴尚京4

作者信息

  • 1. 中山大学 地球科学与工程学院,广东 珠海 519082||广东省地质过程与矿产资源探查重点实验室(中山大学),广东 珠海 519082
  • 2. 香港大学 地球科学系,香港 999077
  • 3. 中国科学技术大学 地球和空间科学学院,合肥 230026||中国科学院壳幔物质与环境重点实验室(中国科学技术大学),合肥 230026
  • 4. 衡阳师范学院 地理与旅游学院,湖南 衡阳 421002
  • 折叠

摘要

Abstract

The Lüliang Group is situated in the central part of the Trans-North China Orogen(TNCO),North China Craton.Investigations of the formation age and tectonic setting of the group are helpful for understanding Neoarchean-Paleoproterozoic regional tectonic evolution.Petrography,geochemistry,and zircon U-Pb dating are combined to study meta-sedimentary and meta-volcanic rocks in the Lüliang Group.The findings reveal that the maximum depositional ages of meta-sedimentary rock samples are~2 510 Ma(Yuanjiacun Formation)and~2 443 Ma(Peijiazhuang Formation),while the crystallization ages of meta-volcanic rock samples are~2 369 Ma(Jinzhouying Formation)and~2 187 Ma(Dujiagou Formation).These new data,combined with previous geochronological studies,imply that the Lüliang Group can be separated into lower and upper sections.The Yuanjiacun and Peijiazhuang Formations of the lower part consist of meta-sedimentary rocks,and were mainly deposited in the late Neoarchean to early Paleoproterozoic.The Jinzhouying and Dujiagou Formations of the upper part are composed of meta-volcanic rocks,and formed in the mid-Paleoproterozoic.Geochemical data show that the meta-sedimentary rocks in the Lüliang Group may have been sourced from acidic magmatic rocks in an active continental margin,while the protoliths of the metamorphic mafic volcanic rocks are likely arc volcanic rocks.Thus,the Lüliang Group may have formed in an active continental margin.The Lüliang Group is similar in age to the late Neoarchean to mid-Paleoproterozoic arc-related magmatic rocks in the Lüliang-Yunzhongshan area and the TNCO,indicating that the orogen may have originally been a long-lived magmatic arc.

关键词

新太古代—古元古代/活动大陆边缘/吕梁群/华北克拉通/锆石U-Pb定年

Key words

Neoarchean-Paleoproterozoic/active continental margin/Lüliang Group/North China Craton/zircon U-Pb dating

分类

天文与地球科学

引用本文复制引用

卢成森,钱加慧,尹常青,张健,高彭,吴尚京..华北克拉通中部造山带吕梁群的形成时代与构造环境[J].成都理工大学学报(自然科学版),2025,52(3):523-541,19.

基金项目

国家自然科学基金项目(42325205,42372227,42025204,41972197) (42325205,42372227,42025204,41972197)

湖南省教育厅重点项目(22A0499). (22A0499)

成都理工大学学报(自然科学版)

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