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首页> 外文期刊>Marine and Petroleum Geology >Submarine channel network evolution above an extensive mass-transport complex: A 3D seismic case study from the Niger delta continental slope
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Submarine channel network evolution above an extensive mass-transport complex: A 3D seismic case study from the Niger delta continental slope

机译:潜艇渠道网络演变以上广泛的大规模运输复合体:尼日尔三角洲大陆坡度的3D地震案例研究

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摘要

A submarine channel network, named Abalama Channel System (ACS), has been recognised in the subsurface of the Niger Delta continental slope. It overlies a mass-transport complex (MTC) and consists of six channel segments, delimited by five avulsion points and one confluence point. High-resolution 3D seismic data are used to investigate the development of the ACS and to describe the interaction between the channels and the underlying MTC. The MTC mainly consists of highly disaggregated materials (MTC matrixes) and in plan-view has a very complex fingered geometry, characterised by the presence of erosional remnants (remnant blocks). The different character of the MTC matrixes compared to that of the remnant blocks likely resulted in a bathymetry characterised by negative and positive relief, which provided the initial confinement for the channels of the ACS. In areas where the MTC-induced confinement was weak or decreased abruptly, channels tended to develop higher sinuosity, increasing channels instability and ultimately causing avulsions. Three ideal categories of submarine channel avulsions are observed. Type 1 is characterised by parent and avulsion channel having similar size and maturity; Type 2 is characterised by a large, high-maturity parent channel and a small, low-maturity avulsion channel; Type 3 emphasizes the larger scale and higher maturity of the avulsion channel compared to the parent channel. In the distal part of the study area, topography related to mud diapirs provided lateral confinement that captured flows avulsed at different times resulting in a channel confluence phenomenon. Submarine channel network evolution recorded by avulsion and confluence points represents an important research theme in deep water sedimentology, as it controls the final distribution of sediments and the extension of sands in the whole deep-water depositional system; hence this study can be used to guide hydrocarbon exploration in analogue systems.
机译:DimerAline频道网络命名为Abalama Channel系统(ACS),已在尼日尔三角洲大陆坡的地下识别。它覆盖着大规模传输复合物(MTC),并且由六个沟道区段组成,偏离五个撕裂点和一个汇合点。高分辨率3D地震数据用于调查ACS的开发并描述通道与底层MTC之间的相互作用。 MTC主要由高度分解的材料(MTC矩阵)和平面图具有非常复杂的指成几何形状,其特征在于存在侵蚀残余(残余块)。与残余块相比,MTC矩阵的不同特征可能导致具有负且正浮雕的浴约定,这为ACS的通道提供了初始限制。在MTC诱导的限制弱或突然下降的区域中,渠道倾向于发展更高的秩序,增加通道不稳定性并最终导致疏散。观察到三种理想的潜艇通道牵引。类型1的特征在于具有相似尺寸和成熟的父母和撕脱通道;类型2的特征在于大,高成熟的母通道和小型低成熟度的牵伸通道;与父频道相比,3型强调撕脱通道的较大规模和更高成熟度。在研究区域的远端部分中,与泥浆有关的地形提供了横向限制,即捕获在不同时间的捕获流动导致通道汇合现象。 Avulsion和Confluence Points记录的潜艇通道网络演进是深水沉积物中的一个重要研究主题,因为它控制了整个深水沉积系统中沉积物的最终分布和砂岩的延伸;因此,该研究可用于在模拟体系中引导碳氢化合物探索。

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