RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 21, ES1003, doi:10.2205/2020ES000723, 2021
Figure 3. Map of the coverage of the Vistula Lagoon with geoacoustic profiles with a two-channel Knudsen Chirp 3212 profilograph (3.5–210 kHz) and the location of sampling stations (above); geoacoustic signs (acoustic transparency) of gas saturation of bottom sediments of the Vistula Lagoon, obtained on a profile through the GNO station.
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