Journal of the Geological Society of Korea, vol.48, pp.79-91, 2012 (ESCI)
Analysis of high-resolution seismic profiles and sediment core was conducted to investigate the
physical and acoustic property of gas-bearing sediments in Yeosu Bay, the South Sea of Korea. Acoustic anomalies
associated with shallow gas are widely distributed in the bay and can be divided into two types. Type I has a very
strong and shallow top reflection that is parallel to the seafloor, with acoustic blanking or turbidity of inner
stratigraphy. Type II is characterized by a sharp top reflection along the seafloor. Physical property and textures
of sediment core that penetrate the gas-bearing zones, show no significant downcore variation regardless existence
of gas bubbles. However, velocity dramatically decreases from average 1497 m/s to 1348~1404 m/s at the
gas-bearing zone. C/N ratios (8.3~12.0) of the organic matter in the cored sediments suggests mixed marine and
terrestrial sources.