Re-division about Fulu Formation and Fulu Interglacial Epoch in Hunan-Guizhou-Guangxi Border Area in South China  

• 责任者：Lin Shuji (Guizhou Academy of Geological Survey ; Guiyang 550005 ; China) ; Xiao Jiafei
• 刊名：Geological Bulletin of China
• 出版年：2010
• 卷期：29(2/3)
• 关键词：南华纪 ; Nanhua Period ; 间冰期环境 ; interglacial environment ; 湖南 ; Hunan Province ; 贵州 ; Guizhou Province ; 广西 ; Guangxi
• 页码：p.195-204
• 图表：3 illus., 1 table, 16 refs.
• 分类号：1400
• issnNo：ISSN1671-2552
• isbnNo：CN11-4648/P

The region which Fulu Formation stratotype section is situated at is the one of the preference places of Nahua System stratotype section in Hunan-Guizhou-Guangxi border region in South China. Fulu interglacial epoch can be divided into three warm climate periods and two icy climate periods. They are named as Sanjiang intersatial, Longjia icy stage, Lanyang intersatial, Liangjiehe icy stage and Datangpo intersatial. The strata corresponded with Fulu interglacial is Fulu Formation. It is divided into five members which are Sanjiang Member, Longjia Member,Lanyang Member, Liangjiehe Member, Datangpo Member. After studing Gucheng Formation stratotype section in Changyang, Hubei Province and Tiesiao Formation stratotype section in Datangpo, Songtao County, Guizhou Province, it showed that both Gucheng Formation and Tiesiao Formation were formed in later Fulu interglacial epoch.