Interferometric interpolation of missing seismic data

Interferometric interpolation of missing seismic data
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DOI:
10.1190/1.3110072
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发表时间:
2009-04
期刊:
影响因子:
3.3
通讯作者:
Yibo Wang;Yi Luo;G. Schuster
Yibo Wang;Yi Luo;G. Schuster
中科院分区:
地球科学2区
文献类型:
--
作者:
Yibo Wang;Yi Luo;G. Schuster

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我们开发了一种干涉插值方法来填充共射孔道的道隙。执行有两个步骤。首先,通过在镜头集合中交叉关联记录的轨迹,然后将所有镜头位置上的相关轨迹对相加,在轨迹间隙中创建虚拟轨迹。其次,将一维匹配滤波器应用于预测事件以校正小波和幅度畸变。通过一维假设(假设在共中点(CMP)集束中点周围有层状介质),干涉插值方法可以应用于CMP集束。它是一种完全数据驱动的方法,只需要原始数据。综合数据和现场数据的经验结果表明,近偏移迹线可以插值;但是由于有限的记录光圈所引入的近似,仍然存在一些伪影。为了比较,我们还使用了二维非平稳预测误差滤波器(PEF)来代替一维匹配滤波器。
We have developed an interferometric interpolation method for filling in trace gaps in common-shot gathers. There are two steps for implementation. First, virtual traces are created in the trace gaps by crosscorrelating recorded traces in a shot gather followed by summing correlated trace pairs over all shot positions. Second, a 1D matching filter is applied to the predicted events to correct for wavelet and amplitude distortions. By using a 1D assumption (assuming a layered medium around the midpoint in a common-midpoint (CMP) gather), the interferometric interpolation method can be applied to CMP gathers. It is a fully data-driven method that requires only the original data. Results with synthetic and field data empirically show that the near-offset traces can be interpolated; but because of the approximations introduced by a limited recording aperture, there are still some artifacts. For comparison, a 2D nonstationary prediction-error filter (PEF) was also used instead of a 1D matching filter in the se...