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1.OUTCROP STUDY ON CONFIGURATIONS AND RESERVOIR HETEROGENEITY IN MEANDERING CHANNEL SANDBODY-An Example from Outcrop Sandbody of Yanan Formation in Northeastern Erdos Basin.
曲流河道砂体内部构成及储集层非均质性的露头研究——以鄂尔多斯盆地东北部延安组露头砂体为例收藏指正
2.Computed results show that:a real anticyclonic meandering path of the Kuroshio appears west of the Bashi Channel(BC),and a tongue with relatively high temperature and salinity spreads into SCS from BC which represents a intrusion of the Kuroshio.
计算结果表明 :黑潮在巴士海峡以西呈一反气旋弯曲流动路径 ,有一相对高温高盐的水舌从巴士海峡伸入南海 ,表明有部分黑潮水侵入南海 .收藏指正
3.Effect of lateral accretion sandbodies of channel sands on the distribution of remaining oil-taking high-sinuosity meandering river of 3 -4 sand groups in upper Ng of Gudao oilfield as exam- ple
河道砂侧积体对剩余油分布的影响——以孤岛油田馆上段3~4砂组高弯度曲流河为例收藏指正
4.The sediments of the incised valleys show an upward-fining succession, and can be grouped into four sedimentary fades: gravel lag-deposit of in-channel to partly over bank sediments of a meandering river, flood plain-estuary, estuary-shallow marine, and estuary sand bar, based on lithology, paleontology, and sedimentary textures and structures.
根据岩石学、沉积结构和沉积构造特征,本区下切河谷充填沉积物具有向上变细的沉积层序,可以划分为4个沉积相类型:河床滞留沉积物到部分曲流河沉积体系的边滩沉积、河漫滩-河口湾沉积、河口湾-浅海沉积和河口湾砂坝沉积。收藏指正
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