青海玉树囊谦第三纪盆地岩相古地理研究
Sedimentary facies and palaeogeography features of Nangqian Tertiary basin in Yushu district, Qinghai
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摘要: 从盆地沉积特征及地层古生物入手,通过分析早第三纪囊谦盆地气候环境,认为属湿润多雨的热带-亚热带气候。盆地岩相古地理揭示,盆地早期为反映构造活动强烈的冲积扇-辫状河三角洲-湖泊沉积组合;晚期为反映构造稳定的河流-湖泊-小型扇三角洲沉积组合。Abstract: Through studying features of sedimentary and stratigraphic paleontology in Nangqian Tertiary basin,the authors point out the climate at Early Tertiary in basin is tropical-subtropical and rainy,the basin is not more than 1 000 m above sea level.The sedimentary faces and palaeogeography discover that in early basin development sedimentary assemblage is fan-braided-delta-lake which reflects tectonic active;in mature basin development the sedimentary assemblage is river-lake-delta.