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《Journal of Palaeogeography》 2011-02
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Morphology and characteristics of deep water high sinuous channel-levee system

Li Hua He Youbin Wang Zhenqi School of Geosciences,Yangtze University,Jingzhou434023,Hubei  
High sinuous channel-levee system with morphology similar to the meandering river has been found during the submarine fan study and hydrocarbon exploration.This system is different from submarine fan in the aspect of morphology and sedimentary characteristics.Based on the achievements from the foreign and domestic researches,combining with the practical researches on gravity flow,a further research on the sedimentary model and sedimentary characteristics of the system has been carried out,including comparison to the meandering river with sedimentary environment,type of flow,morphology and so on.Channel,abandoned channel,levee,crevasse splay and lobe are included in the system.The number of branch of the channel is less,but always be high sinuous.The lithology of channel is mostly sandstone,while conglomerate can be found locally.The main lithology of levee is fine-sand or siltstone while lobe mudstone intercalated with sandstone.The whole morphology of the system is band-belt-like.The discovery and research on the deep water high sinuous channel-levee system not only enrich the content of the deep water deposition study,but also provide a new prospect for oil and gas exploration.
【Fund】: “十一五”国家科技重大专项(编号:2008ZX05030-03-01);; 国家自然科学基金项目(编号:40672071、41072086)联合资助
【CateGory Index】: P618.13
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