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Deep crustal imaging by wide-angle seismic data using seismic interferometry and prestack depth migration.

机译:使用地震干涉法和叠前深度偏移通过广角地震数据进行深地壳成像。

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摘要

Pre-stack depth migration (PSDM) of wide-angle seismic reflection and refraction survey data has a potential to image deep reflectors because the amplitude from a deep reflector becomes large at large offset. However, PSDM of wide-angle data has rarely been applied to the actual data because practical wide-angle surveys are usually too sparse to apply the PSDM. Seismic Interferometry (SI) can dramatically change the situation. By applying the SI to the wide-angle (OBS-airgun) data set, pseudo and dense receiver gathers can be generated. In this study, we generated pseudo receiver gathers by applying SI to the actual OBS-airgun data obtained in the North-Western Pacific region, and we tried to image oceanic Moho, which was about 12 km below the sea surface, by applying PSDM. We conducted a large number of parameter tests, and succeeded in imaging the oceanic Moho.
机译:广角地震反射和折射测量数据的叠前深度偏移(PSDM)具有对深反射层成像的潜力,因为来自深反射层的振幅在较大偏移时会变大。但是,广角数据的PSDM很少应用于实际数据,因为实际的广角测量通常稀疏而无法应用PSDM。地震干涉法(SI)可以大大改变这种情况。通过将SI应用于广角(OBS-气枪)数据集,可以生成伪和密集的接收器集合。在这项研究中,我们通过将SI应用于在西北太平洋地区获得的实际OBS气枪数据来生成伪接收器集,并且我们尝试通过应用PSDM对海平面以下约12 km的海洋莫霍面成像。我们进行了大量参数测试,并成功地对海洋莫霍面成像。

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