• 责任者：Feng Le (School of Resources and Geosciences ; China University of Mining and Technology ; Xuzhou 221116 ; China) ; Dou Luxing
• 刊名：Sedimentary Geology and Tethyan Geology
• 出版年：2013
• 卷期：22(2)
• 关键词：风暴沉积 ; tempestite deposit ; 江苏 ; Jiangsu Province
• 页码：p.32-39
• 图表：illus., 1 table, 22 refs.
• 分类号：0803
• issnNo：ISSN1009-3850
• isbnNo：CN51-1593/P

The Neoproterozoic storm deposits are well developed in the Zhaowei region, Xuzhou, Jiangsu, and may be grouped into seven depositional sequences in different sedimentary environments. These storm deposits are characterized by scour surface, lag deposits, hummocky cross-bedding and liquefied crinkled bedding. The above- mentioned seven depositional sequences of the storm deposits may also be corresponded with the continuous deposits in the shallow shelf margin-platform foreslope-plafform supratidal environments, and display a close correlation with water depths. Finally a genetic model is proposed for the storm deposits in the Jiayuan Formation.