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Least-squares reverse-time migration with a wavefield-separation imaging condition

机译:最小二乘与波场分离成像条件的反向时间迁移

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Although least-squares reverse-time migration (LSRTM) can improve the resolution of the conventional reverse-time migration (RTM) image, directly imaging steeply-dipping fault zones remains a challenge when the acquisition aperture is limited. We develop a least-squares reverse-time migration method with a wavefield-separation imaging condition to enhance imaging steeply-dipping fault zones. Unlike the conventional imaging condition that includes the total source and receiver wavefields, our LSRTM with the wavefield-separation imaging condition cross-correlates the wavefields propagating in opposite vertical or horizontal directions. The conventional imaging condition used in LSTRM uses a fixed source wave-field calculated using the initial model for all subsequent iterations, which may not be able to clearly image fault zones. Our new LSRTM accounts for the updated source wavefield in each iteration. Synthetic examples demonstrate that our LSRTM significantly improves the conventional LSRTM image for imaging steeply-dipping fault zones.
机译:虽然最小二乘逆时偏移(LSRTM)可改善常规逆时偏移(RTM)图像的分辨率,直接成像陡倾断裂带仍然是一个挑战当所述获取孔径限制。我们开发了具有波场分离成像条件的最小二乘反向时间迁移方法,以增强成像陡峭浸渍断层区域。与包括总源和接收器波场的传统成像条件不同,我们的LSRTM具有波场分离成像条件的与波场分离成像条件相互关联在相反的垂直或水平方向上传播的波场。在LSTRM中使用的传统成像条件使用使用初始模型计算的固定源波场,用于所有后续迭代,这可能无法清楚地图像故障区域。我们的新LSRTM占每个迭代中更新的源Wavefield。合成例表明,我们的LSRTM显着改善了用于成像陡峭浸渍断层区域的传统LSRTM图像。

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