Abstract
Relocation of the ocean-bottom seismometer (OBS) is a basic step for subsequent inversion of stratigraphic structure. Obtaining sufficient and accurate position information is crucial to the final velocity model. We propose a new OBS relocation method using direct-wave arrival time information and accurate bathymetric data to provide a better starting of seismic velocity tomography. The new method consists of three steps. The first step is to determine the projection position of OBS on the shooting line according to the symmetry of the time-distance curve under the same yaw distance (the distance between ship’s position and the shooting line to the left or right). Next, the depth node closest to the observation time is found in the depth profile as the initial position of OBS in the direction perpendicular to the shooting line, based on the projection position. Finally, the final position of the OBS is determined by gradient grid search with the depth node as the center. In this paper, the feasibility of the proposed method is verified by experiments on model data. Then, the method is used to relocate 8 OBSs in the Southwest Pacific Ocean. The results show that the offset between the deployment position and relocation position is 50–500 m, with an average of 206 m.
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Acknowledgements
Data and samples were collected onboard of R/V “Kexue”, implementing the open research cruise NORC2020-581 supported by NSFC Shiptime Sharing Project (Project Number: 41949581), and Major Research Plan on West-Pacific Earth System Multispheric Interactions (Project Number: 91858215, 91958206), and the Key Research and Development Program of Shandong Province (Grant No. 2019GHY112019).
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Liu, H., Liu, H., Xing, L. et al. A new method for OBS relocation using direct water-wave arrival times from a shooting line and accurate bathymetric data. Mar Geophys Res 43, 20 (2022). https://doi.org/10.1007/s11001-022-09482-0
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DOI: https://doi.org/10.1007/s11001-022-09482-0