刘凌云,唐佐其,田文明,唐婷婷,龙建喜.黔南独山砂岩地貌特征及形成演化[J].贵州地质,2020,37(1):74-79
黔南独山砂岩地貌特征及形成演化
Sandstone Landform Characteristics and Its Formation Evolution in Dushan of South Guizhou
投稿时间:2019-10-22  
DOI:
中文关键词:  砂岩地貌  成因机理  下泥盆统  黔南独山
英文关键词:Sandstone landform  Genetic mechanism  Lower Devonian Series  Dushan in south Guizhou
基金项目:贵州省地矿局科研项目(黔地矿科合[2017]29号)-《贵州独山地区“张家界地貌”地质景观成因研究》。
作者单位
刘凌云 贵州省地质调查院贵州贵阳550081 
唐佐其 贵州省地质调查院贵州贵阳550081 
田文明 贵州省地质调查院贵州贵阳550081 
唐婷婷 贵州省地质调查院贵州贵阳550081 
龙建喜 贵州省地质调查院贵州贵阳550081 
摘要点击次数: 726
全文下载次数: 413
中文摘要:
      黔南独山北东—东部一带广泛出露下泥盆统砂岩,形成了类型丰富的砂岩地貌景观。本文以野外调查为基础,对地貌景观类型及其成因演化机理作了主要分析,认为该区地貌为省内可与张家界媲美的砂岩地貌分布区,具有砂体时代老、演化属幼年期的特征。
英文摘要:
      Lower Devonian sandstone is widely exposed in the northeast-east area of Dushan in south Guizhou, forming a landscape with abundant types of sandstones. Based on the field investigation, this paper mainly analyzes the types of geomorphic landscapes and their genetic evolution mechanism. It is considered that the geomorphology of this area is a sandstone geomorphic distribution area comparable to Zhangjiajie in the province, which has the characteristics of the old age of sand body and the young age of evolution.
查看全文  查看/发表评论  下载PDF阅读器