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Improved Structural Imaging Using Joint Velocity and Q FWI on Ocean Bottom Seismic
- Publisher: European Association of Geoscientists & Engineers
- Source: Conference Proceedings, 81st EAGE Conference and Exhibition 2019, Jun 2019, Volume 2019, p.1 - 6
Abstract
Gas absorption causes anelastic effects (described by the quality factor Q) and is a well-known source of amplitude loss and phase distortion in seismic data. Advances in full waveform inversion technology have recently offered a new possibility to compensate for phase distortion and amplitude loss by a joint update between velocity and the quality factor (Q). Several industrial applications on towed streamer data have recently been published. In this paper we present a new application on a North Sea dataset with gas present in the overburden. The dataset consists of wide azimuth ocean bottom P-wave seismic data, which is particularly favourable for application of FWI. We see that when combined with Q-Reverse Time Migration a good uplift in reservoir imaging is obtained.