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Cases & packages ge0mlib library Documents & manuals Blog en | ru |
Cases & packagesEach package contains a description of the technique for solving some problem in marine geophysical engineering research. The package includes:
The script execution requires installation of GNU Ostave or MatLab. The package contains all the necessary functions to run the script. The versions of the functions correspond to the time the package was created; the latest versions of the functions are contained in the ge0mlib library. |
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Package C05_03. Magnetometer synchronisation (ScanFish)Delays in the ScanFish-QINSy data transmission channel introduce an additional type of measurement inaccuracy associated with the measurement time-referencing errors (synchronisation errors). The artefacts arising due to synchronisation errors are clearly visible as a "saw effect" (high-frequency meander) in the magnetic field gradient plots (the difference between the readings of two magnetic sensors). C05_03_MagT14 pack_r02.7z(C) 2024-2025 N-Sea Offshore B.V. |
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Package C02_06. Z correction (SBP)The "SES Convert Version 2.3.4.0" file converter (and its earlier versions) does not correctly apply Z corrections to Innomar files with *.ses3 extension. This package was originally created to apply Z corrections properly.
C02_06_Sbp02 pack_r03.7z(C) 2025 N-Sea Offshore B.V. |
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Package C04_08. Navigation injection in JSF files (SSS)Incorrect application of the SSS heading and the "Time constant for course smoothing" parameter in SonarWiz can result in a shift of up to several metres in the target coordinates in the sonogram (see C04_07_Improvement SSS positioning accuracy_rev1.0.pdf). |
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Package C03_04. Positioning of streamer receivers by direct wave travel time (HR/UHR)When performing engineering surveys with HR/UHR methods, the following positioning system is often used: GPS receivers are installed on the seismic source and tail buoy, the lead buoy is absent, and the seismic streamer is considered as a thin thread stretched from the tow point to the tail buoy. The coordinates of seismic receivers are determined with a relatively large error, since the dynamics of the movement of the streamer in the water column differs from the movement of a thin thread stretched in the air.
Publication under approval(C) 2025 ROMONA Inc. |
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