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Near-surface structural model for enhanced seismic data acquisition and processing in North-Central Niger Delta

机译:尼日尔北部中部地区增强地震数据采集和处理的近地表结构模型

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Near-surface structural model was geostatistically developed from a sample density of 36 Uphole/LVL survey points to determine the properties of the weathering layer geological materials. Results from the generated Isopachs and Isovels show a dominant 2-weathered layer model with 1-weathered layer model in only five locations, mainly along the escarpment. The average thickness of the weathering layer to the first refractor consolidated layer is 18.84 m with an average velocity of 1791.40 ms~(-1). Weathering thicknesses ranged from 1.3 to 4.7 m, sub-weathering thicknesses from 11.4 to 35.7 m; weathering velocities from 119 to 941 ms~(-1); sub-weathering velocities from 425 to 1665 ms~(-1) and consolidated layer velocities from 1610 to 2208 ms-1. Proper application of these results will prove very useful and reliable for the enhancement of optimization processes during stages of seismic data processing and serve as baseline data for future 4D seismic data acquisition for accurate mapping of the deep underlying structures for oil and gas exploration in the North-Central part of the Niger Delta.
机译:根据36个Uphole / LVL调查点的样本密度,通过地统计学方法开发了近地表结构模型,以确定风化层地质材料的特性。生成的Isopachs和Isovels的结果显示了一个主要的2风化层模型,其中1个风化层模型仅在5个位置(主要沿悬崖)。耐候层至第一折射材料固结层的平均厚度为18.84 m,平均速度为1791.40 ms〜(-1)。风化厚度为1.3至4.7 m,次风化厚度为11.4至35.7 m;风化速度从119到941 ms〜(-1);亚风化速度为425至1665 ms〜(-1),固结层速度为1610至2208 ms-1。这些结果的正确应用将对增强地震数据处理阶段的优化过程非常有用和可靠,并将作为未来4D地震数据采集的基线数据,以准确绘制北部油气勘探的深层底层结构-尼日尔三角洲的中部。

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