Last glacial sea-level changes and paleogeography of the Korea (Tsushima) Strait

@article{Park2000LastGS,
  title={Last glacial sea-level changes and paleogeography of the Korea (Tsushima) Strait},
  author={Soo chul Park and Dong G. Yoo and C.-W. Lee and Eunil Lee},
  journal={Geo-Marine Letters},
  year={2000},
  volume={20},
  pages={64-71}
}
Abstract The Korea (Tsushima) Strait is an important seaway through which the warm Tsushima Current flows into the East Sea (Japan Sea). A paleogeographic map constrained by a regional sea-level curve developed on the basis of a number of recent 14C radiocarbon dates suggests that the Korea Strait was not closed during the last glacial period. Rather, it was open as a channel-like seaway linking the western North Pacific and the East Sea. Some fraction of the paleo-Tsushima Current inflow… Expand
Holocene evolution of depositional processes off southwest Japan: Response to the Tsushima Warm Current and sea-level rise
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This study presents a review of extensive literature and reports new findings extracted from previously collected cores. Globally lowered sea level during the last glacial maximum (LGM) reduced theExpand
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Abstract The mid-shelf of the southern sea of Korea (Korea Strait) is covered by a series of shore-parallel sand ridges up to 63 km long, 3–9 km wide, and 22 m thick. The ridges are a moribund typeExpand
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