• 责任者：Zheng Ning (Institute of Geology ; Chinese Academy of Geological Sciences ; Beijing 100037 ; China) ; Li Tingdong
• 刊名：Geology in China
• 出版年：2011
• 卷期：38(6)
• 关键词：flysch ; 沉积构造 ; sedimentary structure ; 构造环境 ; tectonic setting ; 江西 ; Jiangxi Province
• 页码：p.1454-1466
• 图表：8 illus., 32 refs.
• 分类号：0803
• 出版序号：20122206
• issnNo：ISSN1000-3657
• isbnNo：CN11-1167/P

Based on the theories of sedimentary geology and lithofacies-paleogeography, the authors combined field investigation with indoor laboratory analysis and recovered the sedimentary-tectonic environment through the analysis of stratigraphic framework, basic characteristics of sandstone and lithofacies. It is supposed that this set of flysch is hemipelagic submarine fan facies rock accumulated rapidly in the southwestern Jiangxi Province. The provenance of the submarine fan was derived from Cathaysia Block in the southeastern Jiangxi Province and then deposited continually in the continental rise on the northern edge of Cathaysia Block. The sea water got deeper gradually from SE to NW in Cambrian period.