尼日尔三角洲中北部增强地震数据采集与处理的近地表构造模型

G. Alaminiokuma, J. Amonieah
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引用次数: 10

摘要

利用36个Uphole/LVL测点的样本密度,建立近地表构造模型,确定风化层地质物质的性质。生成的等等线和等等线结果显示,2风化层模式占主导地位,1风化层模式仅在5个位置占主导地位,主要沿着陡坡。风化层至第一折射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 ~ 4.7 m,亚风化厚度为11.4 ~ 35.7 m;风化速度为119 ~ 941 ms -1;亚风化速度为425 ~ 1665 ms -1,固结层速度为1610 ~ 2208 ms -1。这些结果的正确应用将被证明是非常有用和可靠的,可以在地震数据处理阶段加强优化过程,并作为未来四维地震数据采集的基线数据,为尼日尔三角洲中北部的油气勘探提供准确的深层下伏结构测绘。
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Near-surface structural model for enhanced seismic data acquisition and processing in North-Central Niger Delta
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, subweathering thicknesses from 11.4 to 35.7 m; weathering velocities from 119 to 941 ms -1 ; subweathering 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.
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