卢定彪,张德明,骆珊,吴开彬,龚桂源,王文明.湘黔桂毗邻地区南华纪岩相古地理特征及地质意义[J].贵州地质,2024,(1):9-17
湘黔桂毗邻地区南华纪岩相古地理特征及地质意义
Paleogeography Character and Geological Significance of Nanhua Period Lithofacies in Hu'nan- Guizhou-Guangxi Adjoining Area
投稿时间:2023-10-03  
DOI:
中文关键词:  湘黔桂毗邻区  南华纪  沉积相  古地理
英文关键词:Adjoining area of Hunan,Guizhou and Guangxi  Nanhuan Period  Sedimentary facies  Paleogeography
基金项目:贵州省地质三维空间战略调查评价(2019-02号、DKJJ2020-01号)
作者单位
卢定彪 贵州省地质调查院贵州贵阳550081 
张德明 贵州省地质调查院贵州贵阳550081 
骆珊 贵州省地质调查院贵州贵阳550081 
吴开彬 贵州省地质调查院贵州贵阳550081 
龚桂源 贵州省地质调查院贵州贵阳550081 
王文明 贵州省地质调查院贵州贵阳550081 
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中文摘要:
      为了寻找连续完整且有研究价值的南华系剖面、推进南华系建系工作。本文依据对湘黔桂交界地区南华系主要剖面观察研究所获资料,以沉积岩相类型分析、分布特点为线索,划分出了12种沉积岩相类型,在此基础上反演南华纪各主要阶段古地理环境。得出:南华纪湘黔桂交界地区北西侧为古陆、南东侧为南华裂谷盆地,南华纪早晚两个冰期仅在古陆与盆地过渡的浅海地带,也就是现今的湘黔桂交界地区存在连续完整的沉积,连续完整的具研究价值的南华系剖面应在该区域寻找这一结论。
英文摘要:
      The purpose of this article is to find a continuous,complete,and research-worthy Nanhuan section and to promote the establishment of its SystemIn this paper,based on the data obtained from the observation and research of the main sections of the Nanhuan in Hu’nan- Guizhou-Guangxi border area,the types of sedimentary facies and their distribution characteristics,12 types of sedimentary facies are classifiedThe paleogeographic environment of the main stages of the Nanhuan Period has been inverted from thisIt is concluded that the northwestern part of the south China Yangtze area is paleocontinent and the southeast is the rift basin during the Nanhuan PeriodThe two glacial periods(beginning and ending)continuous and complete sedimentation existed only in the transitional shallow sea areas between paleocontinent and basin,that is,the current junction of Hunan Guizhou and GuangxiThe continuous and complete Nanhuan System section with research value can only be found in this area
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