• 责任者：Xiao Dongsheng (China University of Geosciences ; Beijing 100083 ; China) ; Zhou Junjie
• 刊名：Xinjiang Oil & Gas
• 出版年：2009
• 卷期：5(3)
• 关键词：砾岩 ; conglomerate ; 砂岩 ; sandstone ; 泌阳凹陷 ; Biyang Sag
• 页码：p.1-4, 9
• 图表：6 illus., 5 refs.
• 分类号：1003
• issnNo：ISSN1673-2677
• isbnNo：CN65-1253/TE

///Glutenite abounds in the southern actic region of Biyang Depression. Formation of glutenite is under the control of boundary faults, palaeogeomorphology, paleoclimate and deleveling. And, the boundary fault is dominant factor, and its activity determines the size of fans, the location of transform zone controls the supply routes of sources, and further, it affects the features of palaeogeomorphology. The sedimentary framework a big fan on the big ditch, a small fan on the small ditch is concluded. The paleoclimate mainly affects the sediment supply from the source area; The deleveling mainly controls the development of turbidite sandstone. According to the formation mechanism, the distribution rules of glutenite are come to conclusion.