PRE STACK DEPTH MIGRATION UNTUK KOREKSI EFEK PULL UP DENGAN MENGGUNAKAN METODE HORIZON BASED DEPTH TOMOGRAPHY PADA LAPANGAN ‘A1 DAN A2’

JGE Pub Date : 2020-01-17 DOI:10.23960/JGE.V4I1.1055
Atikah Azzahra, Bambang Mujihardi
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Abstract

In the case of seismic data processing with sandstone lithology such as shale and carbonate often get the result of data processing which have pull up effect especially on the time domain migration result. Pre stack depth migration is a processing based on focusing the amplitude according to the actual depth by using the input interval velocity. Migration is performed using kirchhoff pre stack depth migration algorithm. Pre stack depth migration is done with modeling of horizontal based depth tomography method. This method uses residual moveout correction applied along the horizon-picking line. This research uses two field data that is A1 and A2 Field. A1field has characteristics of carbonate rock that produce pull up shaped similar to carbonate layer. A2 field has a pull-up effect that is not very clear but has build up because of the layer above it. Stages performed starting from the processing of pre stack time migration in the form of velocity picking, generate rms velocity and migration time domain. The pre stack depth migration process begins with a velocity transformation with the dix transformation equation to generate interval velocity, migrate Pre stack depth migration, perform horizon interpretations and perform velocity modeling using the horizon based depth tomography method. The iteration is done 4 times and resulted in the final section of pre stack depth migration which has been corrected by pull up effect.
适用时,用于上拉效应校正的叠层深度偏移——基于“A1和A2”路径深度层析成像的地平线方法
在对页岩、碳酸盐岩等砂岩岩性的地震数据进行处理时,往往会得到具有上拉效应的数据处理结果,尤其是对时域偏移结果的影响。叠前深度偏移是基于使用输入的层速度根据实际深度聚焦幅度的处理。使用基尔霍夫叠前深度偏移算法进行偏移。叠前深度偏移采用基于水平的深度层析成像方法建模。该方法使用沿地平线拾取线应用的剩余时差校正。本研究使用了两个领域的数据,即A1和A2领域。A1field具有碳酸盐岩的特征,其产生的上拉形状类似于碳酸盐层。A2场的上拉效应不是很清楚,但由于其上的层而积累起来。从速度拾取形式的叠前时间偏移处理开始执行的阶段,生成均方根速度和偏移时域。叠前深度偏移过程从使用dix变换方程的速度变换开始,以生成层速度,偏移叠前深度迁移,执行层位解释,并使用基于层位的深度层析成像方法进行速度建模。迭代进行了4次,得到了叠前深度偏移的最后一段,并通过上拉效应进行了校正。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
JGE
JGE
自引率
0.00%
发文量
16
审稿时长
22 weeks
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