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| 1 | Review of research in internal-wave and internal-tide deposits of China显示文摘Study of internal-wave and internal-tide deposits is a very young research field in deep-water sedimentology. It has been just twenty years since the first example of internal-wave and internal-tide deposits was identified in the stratigraphic record. Since that time, Chinese scholars have made unremitting efforts and gained some significant research achievements in this field. This paper briefly outlines the history and main achievements of research of internal-wave and internal-tide deposits in China, describes depositional charac-teristics, sedimentary successions, types of lithofacies, and depositional models of internal-wave and internal-tide deposits identified mainly from ancient strata, and summarizes the existing problems in this research field. New advances in marine physics should be applied to research of the subject of internal-wave and internal-tide deposition, whereas the sedimentary characteristics of internal-wave and internal-tide deposits may be used to deduce the physical processes of their creation. Flume experiments on internal-wave and internal-tide deposition should also be put in practice as often as possible, so that the mechanisms of internal-wave and internal-tide deposition can be explored. | Gao Zhenzhong He Youbin Li Xiangdong Duan Taizhong | 2013 | Journal of Palaeogeography2013，2，1： | 9 |
| 2 | Characteristics of internal-wave and internal-tide deposits and their hydrocarbon potential显示文摘内部波浪、内部潮的存款的学习在最后十年期间是 sedimentology 上的一个新研究领域。内部波浪和内部潮导致的深海的拖拉水流在现代的海地板上被开发,它能形成不仅各种小规模和疏开深海的拖拉水流存款,而且在 km 尺寸的大规模沉积波浪可伸缩。在这篇论文,在海洋学的内部波浪和内部潮的概念和特征被介绍,并且特征,沉积序列,沉积 microfacies 和沉积在深海底部发现的内部波浪、内部潮的存款和大规模沉积波浪的起源当模特儿被总结。在内部波浪、内部潮的存款和石油之间的关系被讨论,并且最后内部波浪、内部潮的存款被显示是为石油探索的一个新潜在的领域。 | He Youbin Gao Zhenzhong Luo Jinxiong Luo Shunshe Liu Xuefeng | 2008 | Petroleum Science2008，5，1： | 9 |
| 3 | Lithofacies palaeogeography of the Upper Permian Changxing Stage in the Middle and Upper Yangtze Region,China显示文摘Based on the petrological study,according to single factor analysis and multifactor comprehensive mapping method,the quantitative lithofacies palaeogeography of the Upper Permian Changxing Stage of the Middle and Upper Yangtze Region was studied.The Changxing Stage in the Middle and Upper Yangtze Region is mainly composed of carbonate rocks;in addition,clastic and siliceous rocks occur with rare coals and pyroclastic rocks.Lithofacies can be divided into five types,including clastic rock assemblage,clastic rock-limestone assemblage,limestone assemblage,limestone-siliceous rock assemblage,and siliceous rock-clastic rock assemblage.Four fundamental ecological types and five fossil assemblages were recognized in the Changxing Stage.On the basis of the petrological and palaeoecological study,eight single factors were chosen including thickness,content of marine rocks,content of shallow water carbonate rocks,content of bioclasts with limemud matrix,content of bioclasts with sparry cement,distribution of reefs,content of thin bedded siliceous rocks and content of deep water sedimentary rocks.And eight single factor maps and one lithofacies paleogeographic map of the Changxing Stage were compiled.Paleoenvironments from west to east include an erosional area,fluvial plain,clastic platform,carbonate platform and reefs that developed there,slope and basin,low energy organic banks,and high energy organic banks.Sedimentary environments have an obvious control on the development of the source rocks,and the excellent source rocks are developed in the Dalong Formation.Changxing Stage reservoirs should be dominated by the reef and platform surrounding the GuangyuanLiangping Basin rim area,and is the most favorable exploration area of the reef petroleum reservoirs of the Changxing Formation. | He Youbin Luo Jinxiong Wen Zhan | 2013 | Journal of Palaeogeography2013，2，2： | 4 |
| 4 | Changing color of Chinese loess: Geochemical constraint and paleoclimatic significance显示文摘 | Youbin Sun Liu He Lianji Liang Zhisheng An | 2010 | Journal of Asian Earth Sciences2010，，6： | 1 |
| 5 | Characteristics and origins of deep-sea large-scale sediment wave显示文摘 | He Youbin Luo Jinxiong Xin Changjin | 2007 | Journal of China University of Geosciences2007，，： | 1 |
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