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首页> 外文期刊>Marine and Petroleum Geology >The architecture and evolution of the Middle Bengal Fan in vicinity of the active channel-levee system imaged by high-resolution seismic data
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The architecture and evolution of the Middle Bengal Fan in vicinity of the active channel-levee system imaged by high-resolution seismic data

机译:高分辨率地震数据成像的中孟加拉河扇在主动河道堤防系统附近的构造和演化

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High-resolution seismic data from the Middle Bengal Fan were analysed to study the architecture of the fan in the vicinity of the active channel-levee system and to evaluate channel behaviours.The upper 600 m column of the fan in the study area reveal a pattern of different sized channel-levee systems and high amplitude reflection packets(HARPS)of varying thicknesses,no mass-flow deposits or hemipelagic drapes are found.Within the channel-levee systems,units of chaotic high amplitude reflectors(CHARS),which represent aggraded and migrated channel axes,as well as abandoned channel-fill deposits appear.All channels are characterised by erosional incision into underlying deposits.Within the active channel-levee system,numerous cut-off loops are found showing a broad spectrum of complex behaviours with different ratios of vertical aggradation and lateral migration.As a difference to the Amazon Fan,the floors of all cut off loops and the active channel are not elevated above the surrounding seafloor,which may lead to such a long lifetime resulting in the large number of cut-off loops.In contrast,a detailed studied buried system shows no cut-off loops and is characterised by a more simple behaviour:a first phase of lateral migration is followed by a second phase of simultaneous vertical aggradation and lateral migration,which finally elevated the channel floor above the level of the surrounding seafloor.These architectural differences between the systems indicate that different loaded turbidity currents have built up both systems.The aggrading and migrating channel floors likely have reservoir potential,but a high-resolution 3D seismic survey and drilling are necessary for final proof.
机译:分析了来自孟加拉中部扇的高分辨率地震数据,以研究主动通道-堤坝系统附近的扇的体系结构并评估通道行为。研究区域中扇的上部600 m柱揭示了一种模式大小的通道-堤坝系统和厚度变化的高振幅反射包(HARPS)的分布,没有发现质量流沉积物或半悬垂性。在通道-堤坝系统中,代表聚集的混沌高振幅反射器(CHARS)的单元所有通道均具有侵蚀性切入下伏沉积物的特征。在活动通道-堤坝系统中,发现了许多截止回路,显示了各种不同行为的复杂行为垂直凝结和横向迁移的比率。与亚马逊风扇不同的是,所有切断回路的地板和活动通道的高度均未升高到周围环境之上相比之下,经过详细研究的埋藏系统未显示出任何截止回路,而且其行为更为简单:横向迁移的第一阶段第二阶段是垂直凝结和横向迁移同时进行,这最终使河床底面升高到周围海底水平面以上。这些系统之间的体系结构差异表明,两个系统都形成了不同的负载浊流。通道底可能具有储层潜力,但是高分辨率3D地震勘探和钻探对于最终证明是必要的。

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