Correction of water column height variation on 2D grid high-resolution seismic data using dGPS based methodology
Ayobami Abegunrin1, Daniel A Hepp2, Tobias Mörz2,3
1MARUM - Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany. aabegunrin@marum.de.
A new differential Global Positioning System (dGPS) method precisely corrects seismic data for water column variations. This improves geological interpretations in complex shallow marine environments, enhancing subsurface structure identification.
Area of Science:
- Geophysics
- Marine Geology
- Seismic Data Processing
Background:
- Water column variations (tides, currents, salinity, temperature) complicate high-resolution seismic data correction, especially in shallow marine settings.
- Vessel motion further impacts accurate water column height determination.
- Precise geological interpretations on decimeter scales require robust water column correction methods.
Purpose of the Study:
- To introduce a time-efficient and precise differential Global Positioning System (dGPS) based methodology for water column height correction.
- To improve the tracking and quality of geological interpretations from high-resolution seismic data.
- To apply and validate the methodology in a complex shallow marine environment.
Main Methods:
- Development and application of a dGPS-based methodology for seismic data correction.
- Testing the methodology on geophysical profiles from the German North Sea.
- Analysis of sub-surface sedimentary structures on decimeter scales.
Main Results:
- The corrected seismic profiles revealed a deeper seafloor, consistent with tide-corrected bathymetry data (1.1–3.4 m deeper, mean 2.2 m).
- The correction enabled accurate plotting of Holocene channel base depths and gradients.
- Distinction of glacial and post-glacial valleys and improved stratigraphic framework were achieved.
Conclusions:
- The dGPS-based methodology significantly enhances the accuracy of high-resolution seismic data processing in shallow marine environments.
- This method is crucial for detailed geological interpretations, including stratigraphy and structural framework delineation.
- The approach offers a precise and less time-consuming alternative for seismic data correction.
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