Land Seismic Multiples Detection and Attenuation In Bornu-Chad Basin, Nigeria

Dorathy B. Umoetok, E. Uko, Iyeneomie Tamunobereton-ari, C. Israel-Cookey, Odukokoma N. Ebini
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Abstract

Abstract Three dimensional (3D) seismic survey was acquired and processed in Bornu-Chad basin, Nigeria with the aim of detecting and attenuating multiples to aid proper imaging of the subsurface. The 25.5km2 volume was processed using SeisUp processing software on a 32-Node Cluster Infrastructure (CI) hardware. Considering the imaging objectives and depth of interest of 1.2s-4.5s, the minimum, middle and maximum offsets were set at 500-2300m, 2500-4300m and 4500-7300m respectively. Since the study area comprised of dry open land and swampy Lake Chad, vibroseis and dynamite sources were used respectively. Charge depth was 0m (surface) for vibroseis and 25m dynamite. The dataset was first pre-conditioned, normalized, regularized before application of demultiple process. The detection and demultiple processes based on multiple characteristics of periodicity and velocity discrimination were applied as the multiples have comparable velocity with the primaries. The near-surface reverberations and short-period multiples were attenuated using predictive deconvolution and radon transform algorithms. High resolution radon was performed on post-migrated common-mid-point (CMP) gathers and stacked with 1kmx1km target line velocities. Internal multiples were detected and attenuated using data-driven methodology of extended internal multiple prediction (XIMP). Multiples detected were short, long period and interbed multiples on all frequencies ranges of 0 – 90Hz but useful seismic frequency range was between 20Hz and 70Hz. The frequencies and amplitudes of the primaries and multiples were very comparable, therefore great care was taken in the attenuation processes. The results of this work has produced better seismic section for interpretation of subsurface geology in the study area.
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尼日利亚Bornu Chad盆地陆地地震倍数的探测与衰减
摘要在尼日利亚Bornu Chad盆地采集并处理了三维地震勘探,目的是检测和衰减多次波,以帮助对地下进行正确成像。25.5平方公里的体积使用SeisUp处理软件在32节点集群基础设施(CI)硬件上进行处理。考虑到成像目标和感兴趣深度为1.2s-4.5s,最小、中间和最大偏移分别设置为500-2300m、2500-4300m和4500-7300m。由于研究区域由干燥的开阔地和沼泽的乍得湖组成,因此分别使用了可控震源和炸药源。可控震源和25米炸药的装药深度为0米(表面)。在应用解复用过程之前,首先对数据集进行预处理、归一化和正则化。由于倍数具有与原色相当的速度,因此应用了基于周期性和速度辨别的多重特性的检测和解复用过程。利用预测反卷积和radon变换算法衰减了近地表反射和短周期多次波。在偏移后的共中点(CMP)道集上进行了高分辨率氡测量,并以1kmx1km的目标线速度进行了叠加。使用扩展内部倍数预测(XIMP)的数据驱动方法检测并衰减内部倍数。在0–90Hz的所有频率范围内,检测到的倍数都是短周期、长周期和互层倍数,但有用的地震频率范围在20Hz和70Hz之间。一次波和多次波的频率和振幅非常相似,因此在衰减过程中非常小心。这项工作的结果为研究区的地下地质解释提供了更好的地震剖面。
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