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首页> 外文期刊>Geophysics: Journal of the Society of Exploration Geophysicists >Reverse time migration of multiples for subsalt imaging
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Reverse time migration of multiples for subsalt imaging

机译:盐下成像倍数的逆时偏移

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摘要

Some hydrocarbon reservoirs are trapped beneath saltbodies, where seismic imaging is greatly challenged due topoor illumination. Multiple reflections have different propagationwave paths from primary reflections and thus can beused to complement the illuminations where primary reflectionsfrom beneath the salt are not acquired. Consequently,migration of multiples can sometimes provide better subsaltimages compared to conventional migration which uses primaryreflections only. In this paper,we propose to modify conventionalreverse time migration so that multiples can be usedas constructive reflection energyfor subsalt imaging. Thisnewapproach replaces the impulsive source wavelet with therecorded data containing both primaries and multiples anduses predicted multiples as the input data instead of primaryreflections. In the reverse time migration process, multiplesrecorded on the surface are extrapolated backward in timeto each depth level, and the observed data with both primariesand multiples are extrapolated forward in time to the samedepth levels, followed by a crosscorrelation imaging condition.A numerical test on the Sigsbee2B data set shows thata wider coverage and a more balanced illumination of the subsurfacecan be achieved by migration of multiples comparedwith conventional migration of primary reflections. Thisexampledemonstrates that reverse time migration of multiplesmight be a promising method for complex subsalt imaging.
机译:一些碳氢化合物储集层被困在盐体下面,由于光照不足,地震成像受到很大挑战。多次反射具有与主反射不同的传播波路径,因此可以用于补充没有从盐下获取主反射的照明。因此,与仅使用主反射的常规迁移相比,倍数的迁移有时可以提供更好的盐下图像。在本文中,我们建议修改常规的逆时偏移,以便将倍数用作盐下成像的建设性反射能量。这个新方法用包含原始和倍数的记录数据代替了脉冲源小波,并使用预测的倍数作为输入数据而不是原始反射。在逆时偏移过程中,将在表面上记录的倍数在时间上向后外推到每个深度级别,并将具有原始和倍数的观测数据在时间上外推到相同的深度级别,然后进行互相关成像条件。 Sigsbee2B数据集显示,与传统的一次反射偏移相比,多次偏移可以实现更广泛的覆盖范围和更均匀的地下照明。这个例子说明了多重力的逆时偏移是用于复杂的盐下成像的有前途的方法。

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