• 责任者：Zhao Liangdong (School of Earth Sciences and Resources ; China University of Geosciences ; Beijing 100083 ; China) ; Guo Rongtao
• 刊名：Geology in China
• 出版年：2011
• 卷期：38(3)
• 关键词：早寒武世 ; Lower Cambrian ; 地层格架 ; stratigraphic framework ; 贵州 ; Guizhou Province
• 页码：p.577-585
• 图表：5 illus., 25 refs.
• 分类号：1200
• issnNo：ISSN1000-3657
• isbnNo：CN11-1167/P

 Lower Cambrian strata are quite completely developed in southeast Guizhou Province, and the transitional facies characterized by intense facies change comprise an upward shallowing sedimentary succession, which constitutes a second-order sequence. Based on two kinds of natures of the third-order sequence, i.e., the regularity of lithofacies succession in space and the synchronism of environmental change in time, and taking the two kinds of facies-transition surface and two kinds of diachronisms in stratigraphic records as the fundamental elements in building sequence-stratigraphic framework for the Lower Cambrian strata of the study area, the authors hold that the sequence-stratigraphic framework demonstrates the special third-order sedimentary succession patterns formed after the platform drowning event caused by the rapid transgression at the early stage of Cambrian.