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Wave-Equation Prediction of Multiples – Different Strategies for Different Conditions

机译:倍数的波动方程预测–不同条件下的不同策略

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SRME is the method of preference for data from areas with deep sea-floor, especially when a thick package of strong reflectors is present below the sea-floor. To reconstruct missing traces required by 3D SRME prediction, we use a repositioning of traces based on 3D hyperbolic moveout assumption. We use wave-equation (WE) approach when several orders of multiples are involved. WE approach is especially efficient when the main free-surface multiples are just 'pure' water-layer multiples and peg-legs. WE approach allows us to use different WE prediction schemes based on complexity of structure and in 3D it has less sampling problems than 3D SRME. In our WE approach all source-side and receiver-side multiples of all orders are suppressed simultaneously in one consistent step. The prediction and adaptive subtraction of multiples are performed in the same domain, therefore no additional sorting or additional transformations are required.
机译:SRME是从海底深处获取数据的首选方法,特别是当海底下有厚厚的强反射体包裹时。为了重建3D SRME预测所需的丢失迹线,我们使用了基于3D双曲偏移假设的迹线重新定位。当涉及多个数量级的倍数时,我们使用波动方程(WE)方法。当主要自由表面倍数只是“纯”水层倍数和桩腿时,WE方法特别有效。 WE方法允许我们根据结构的复杂性使用不同的WE预测方案,在3D模式下,其采样问题少于3D SRME。在我们的WE方法中,所有订单的所有源方和接收方倍数都在一个一致的步骤中同时被抑制。倍数的预测和自适应减法在同一域中执行,因此不需要其他排序或其他变换。

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