• 责任者：Xing Zhifeng (Key Laboratory of Biogenic Traces and Sedimentary Minerals of Henan Province ; Institute of Resources and Environment ; Henan Polytechnic University ; Jiaozuo 454003 ; China) ; Qi Yong’an
• 刊名：Acta Sedimentologica Sinica
• 出版年：2011
• 卷期：29(5)
• 关键词：生物成因构造 ; biogenic structure ; 微生物 ; microorganisms ; 藻席构造 ; algal structure ; 河南 ; Henan Province
• 页码：p.857-864
• 图表：5 illus., 28 refs.
• 分类号：0803
• 出版序号：1705
• issnNo：ISSN1000-0550
• isbnNo：CN62-1038/P

Yunmengshan Formation, belonging to Mesoproterozoic Ruyang Group, lies in the southern margin of North China Platform and consists mainly of silicic clastic sedimentary successions. Microbially Induced Sedimentary Structures (MISS) occur on the surface of purple or yellow sandstone interbedded with mudstone or siltstone, especially on junction surface between sandstone and mud lamination. In the further investigation of thin-sections, five types of microstructures have been found: wavy crinkled laminae, network fabrics, mat layer bound small grains, mat layer bound heavy minerals and oriented grains. Microstructures could be used to reconstruct small-scaled facies within coastal environments.