Palaeozoic-Mesozoic Sedimentary Evolution Characteristics of the Xuefeng Mountain
详细信息
- 责任者：Li Cong (College of Geo-Resources and Information ; CUP ; Qingdao 266555 ; China) ; Chen Shiyue
- 刊名：Geology in China
- 出版年：2011
- 卷期：38(1)
- 关键词：震旦纪 ; Sinian ; 三叠纪 ; Triassic ; 沉积演化 ; sedimentary evolution ; 古生代 ; Paleozoic ; 华南地区 ; South China
- 页码：p.43-51
- 图表：7 illus., 1 table, 27 refs.
- 分类号：0803
- issnNo：ISSN1000-3657
- isbnNo：CN11-1167/P
摘要
In this paper,the authors studied the characteristics of Palaeozoic-Mesozoic stratigraphic sedimentation in the Xuefeng Mountains and its lateral layers by means of field investigation and indoor analysis, and found out the regularity of uplifting-depression change in the Xuefeng Mountains since Palaeozoic. The course of tectono-sedimentary evolution from Palaeozoic to Mesozoic can be divided into five phases according to the features of uplifting-depression change and the palaeogeographic property in Xuefeng area. The authors confirmed that the Xuefeng’s evolution is characterized by a polyphase compounding folded intracontinental orogenic belt, rather than an "ancient land".