The Sedimentary Characteristics, Evolution and Controlling Factors of Southern Margin, Yangtze Carbonate Platform during the Hercynian-Indosinian Stage oft-com:office:office" />
详细信息
- 责任者：Shi Guo (Institute of Sedimentary Geology ; Chengdu University of Technology ; Chengdu 610059 ; China) ; Tian Jingchun
- 刊名：Geoscience
- 出版年：2009
- 卷期：23(6)
- 关键词：碳酸盐岩 ; carbonate rocks ; 沉积体系 ; depositional system ; 扬子地区 ; Yangtze Region
- 页码：p.1113-1120
- 图表：6 illus., 1 table, 18 refs.
- 分类号：0803
- issnNo：ISSN1000-8527
- isbnNo：CN11-2035/P
摘要
The carbonate platform developed on the Yangtze block during the Hercynian-Indosinian stage. Platform margin depositional system developed in the southern carbonate platform including four sedimentary types: the beach of carbonate platform margin, the reef platform of carbonate platform margin, platform margin slope and the sea between beach (reef). The study proved that horizontal migration of platform margin was mainly controlled by syndepositional faults, the vertical sequence evolution of platform margin was mainly controlled by sea-level change, the type of margin reef-bank was controlled by different types of carbonate secret organisms. oft-com:office:office" />