• 责任者：Wang Xiaofei (Chengdu Institute of Geology and Mineral Resources ; Chengdu 610081 ; China)
• 刊名：Sedimentary Geology and Tethyan Geology
• 出版年：2013
• 卷期：33(1)
• 关键词：志留纪 ; Silurian ; 沉积构造 ; sedimentary structure ; 湖南 ; Hunan Province
• 页码：p.49-54
• 图表：illus., 5 refs.
• 分类号：1200
• issnNo：ISSN1009-3850
• isbnNo：CN51-1593/P

The measured Wentang Silurician section in Zhangjiajie lies in the area west of the Hunan. Prior to the Silurician, the Xuefengshan area was once uplifted and graded into the land. Wuling uplift in The expansion of the Xuefengshan uplift during the Silurician led to the transition of the study area from shallow marine to littoral environments, and even to the land in the area west of the Cili-Baojing zone till the end of the Late Silurician. The evolution of sedimentary sequences and sedimentary facies indicated by the Wentang Silurician section in this area noticeably displays the coupling relationship with the evolution of the Wuling uplift. The Upper Silurician - Lower and Middle Devonician stratigraphic records are absent in the measured section.