日本地球惑星科学連合2018年大会

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[EE] 口頭発表

セッション記号 S (固体地球科学) » S-TT 計測技術・研究手法

[S-TT47] Recent Advances in Exploration Geophysics (RAEG2018)

2018年5月24日(木) 10:45 〜 12:15 A11 (東京ベイ幕張ホール)

コンビーナ:三ケ田 均(京都大学大学院工学研究科)、飯尾 能久(京都大学防災研究所)、島 伸和(神戸大学大学院理学研究科惑星学専攻、共同)、武川 順一(京都大学大学院工学研究科)、座長:武川 順一三ケ田 均

11:15 〜 11:30

[STT47-09] Separation of migration and tomography modes of full-waveform inversion in the plane-wave domain

*di wu1GANG YAO2 (1.China University of Petroleum、2.IMPERIAL COLLEGE LONDON)

キーワード:full-waveform inversion, migration mode, tomographic mode, mode separation, plane wave domain, angle filtering

Full-waveform inversion (FWI) includes both migration and tomography modes. The migration mode acts like a non-linear least-squares migration to build the model interfaces with reflections while the tomography mode behaves as tomography to correct the background velocity. The migration mode is the main response of inverting reflections while the tomography mode exists in response to inverting both the reflections and refractions. To emphasize one of the two modes in FWI, especially for inverting reflections, the separation of the two modes in the gradient of FWI is required. Here, we will present a new method to achieve this separation by angle-dependent filtering in the plane-wave domain. Firstly, the source and residual wavefields are transformed into the plane-wave domain by Fourier transform; secondly, the tomography and migration components are distinguished by the opening angle between the plane-waves of the transformed source and residual wavefields. The opening angles close to 180° contribute to the tomography component while the others correspond to the migration component. This method is not affected by velocity variation, the dip angle of reflectors, the direction of wave propagation or anisotropy. It, therefore, is very effective and robust. This is demonstrated by theoretical analysis, synthetic and field data examples.