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首页|期刊导航|地质通报|对湖北大洪山地区一套紫红色砂-砾岩系沉积年代的再认识--碎屑锆石U-Pb年龄及其地质意义

对湖北大洪山地区一套紫红色砂-砾岩系沉积年代的再认识--碎屑锆石U-Pb年龄及其地质意义

张雄 曾佐勋 潘黎黎 曾智辉 彭练红 徐大良 魏运许 刘浩 邓新

地质通报2016,Vol.35Issue(7):1069-1080,12.
地质通报2016,Vol.35Issue(7):1069-1080,12.

对湖北大洪山地区一套紫红色砂-砾岩系沉积年代的再认识--碎屑锆石U-Pb年龄及其地质意义

Recognition of the sedimentation age of a series of purple-red colored glutenite sedimentary rocks in Dahong Mountain area, northern Hubei Province:Detrital zircon U-Pb geochronology and its geological significance

张雄 1曾佐勋 2潘黎黎 1曾智辉 1彭练红 1徐大良 3魏运许 3刘浩 3邓新3

作者信息

  • 1. 中国地质大学 武汉 地球科学学院华中构造力学研究中心,湖北武汉430074
  • 2. 重庆地质矿产研究院,重庆400042
  • 3. 中国地质调查局武汉地质调查中心,湖北武汉430223
  • 折叠

摘要

Abstract

The sedimentary age of a series of purple-red colored glutenite sedimentary rocks in Dahong Mountain area of northern Hubei Province is controversial. Some researchers hold that it is of late Jurassic period, while others believe it is of early Nanhua peri⁃od. In this paper, the authors studied detrital zircon geochronology of this layer and obtained 125 groups of effective age data which range from 3223Ma to 771Ma, and the age data are focused on three periods: late Neo-Archean to early Paleoproterozoic (~2500Ma), Paleoproterozoic (~2000Ma), and Neoproterozoic (~800Ma). The authors compared the petrological features and the detri⁃tal zircon age distribution of Liantuo Formation in southeastern Hubei, Three Gorges area, and the purple-red colored glutenite. It is considered that the Liantuo Formation in southeastern Hubei, Three Gorges area and the purple-red colored glutenite have similar sources. The sedimentary age of this series of purple-red colored glutenite sedimentary rocks in Dahong Mountain area of northern Hubei Province is early Nanhua period rather than the late Jurassic period. Based on a comprehensive analysis of the Precambrian age of Yangtze block, the authors hold that there may exist lots of Neo-Archean to early Paleoproterozoic concealed rocks, and the rocks around 2500Ma may be an important part of the basement of Yangtze block. There existed a magmatic activity around 2000Ma in Yangtze block, and it may be connect to the aggregate event of Columbia supercontinent. There is a Neoproterozoic rift on the northern margin of Yangtze block, which might be connected to the breakup of Rodinia supercontinent, and the basic rock was probably the source of the mafic gravel in the purple-red colored glutenite sedimentary rocks.

关键词

莲沱组/碎屑锆石/LA-ICP-MS锆石U-Pb年龄/扬子地块/大洪山

Key words

Liantuo/Formation/LA-ICP-MS zircon U-Pb ages/Yangtze block/Dahong Mountain

分类

天文与地球科学

引用本文复制引用

张雄,曾佐勋,潘黎黎,曾智辉,彭练红,徐大良,魏运许,刘浩,邓新..对湖北大洪山地区一套紫红色砂-砾岩系沉积年代的再认识--碎屑锆石U-Pb年龄及其地质意义[J].地质通报,2016,35(7):1069-1080,12.

基金项目

中国地质调查局项目 ()

地质通报

OA北大核心CSCDCSTPCD

1671-2552

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