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Late Quaternary Seismic Stratigraphy and Sedimentation of the Southeastern Continental Shelf, Korea Strait  

Yoo Dong-Geun (Petroleum and Marine Resources Division, Korea Institute of Geoscience and Mineral Resource)
Lee Chi-Won (Petroleum and Marine Resources Division, Korea Institute of Geoscience and Mineral Resource)
Min Gun-Hong (Petroleum and Marine Resources Division, Korea Institute of Geoscience and Mineral Resource)
Lee Ho-Young (Petroleum and Marine Resources Division, Korea Institute of Geoscience and Mineral Resource)
Choi Joung-Gyu (Petroleum and Marine Resources Division, Korea Institute of Geoscience and Mineral Resource)
Park Soo-Chul (Oceanography Department, Chungnam National University)
Publication Information
Geophysics and Geophysical Exploration / v.8, no.3, 2005 , pp. 201-206 More about this Journal
Abstract
Interpretation of high-resolution seismic profiles from the southeastern continental shelf of Korea reveals that the sedimentary deposits consist of seven seismic units formed during the late Quaternary. These units comprise lowstand, transgressive, and highstand systems tracts. The lowstand systems tract consists of a lowstand prograding wedge (SU1) and a mass flow deposit (SU2) including slumps and slides. The transgressive systems tract contains four seismic units: an ancient beach/shoreface deposit (SU3), a channel-fill deposit (SU4), a transgressive sand layer (SU5), and a transgressive sand ridge (SU6). The highstand systems tract consists of an inner-shelf mud deposit (SU7) derived from the Nakdong and Seomjin rivers during the last 6 ka when sea level was close to the present level.
Keywords
Late Quaternary; Seismic stratigraphy; Sea-level changes; Korea Strait;
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