西非陆坡区深水复合水道沉积构型模式OA北大核心CSCDCSTPCD
Sedimentary architecture model of deep-water channel complexes in slope area of West Africa
依据浅层高频地震和深层钻井资料,通过分析地震相外部几何形态、内部反射特征以及相干体属性地层切片,对西非陆坡深水区复合浊积水道的沉积构型模式进行研究.结果表明:西非陆坡深水区复合浊积水道沉积构型模式可概括为复合水道间的垂向叠置模式和侧向叠置模式、复合水道内部单一水道间的平面迁移模式和剖面迁移模式；复合水道间的垂向叠置模式包括孤立式、叠加式和切叠式3种类型,侧向叠置模式包括叠合式和分离式两种类型；复合水道内部单一水道间存在侧向和沿古流向两种迁移模式.
Based on shallower-layer high resolution 3D seismic data and deep-layer drilling data, the sedimentary architecture model of turbidite channel complexes in deepwater slope area of West African was studied by the research of external morphology, the internal amplitude characteristics of seismic facies, as well as the analysis of coherence cube stratigraphic slices. The results show that the model can be generalized for two types. One is vertical and lateral s…查看全部>>
赵晓明;吴胜和;刘丽
西南石油大学资源与环境学院,四川成都610500成都理工大学油气藏地质及开发工程国家重点实验室,四川成都610500中国石油大学地球科学学院,北京102249
能源科技
西非陆坡区复合水道单一水道构型模式
slope area of West Africa channel complex single channel architecture model
《中国石油大学学报（自然科学版）》 2012 (6)
1-5,12,6
油气藏地质及开发工程国家重点实验室(成都理工大学)开放基金资助项目(PLC201203)国家科技重大专项(2011ZX05030-005-02)
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