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

被引：0
|
作者：
S.-C. Park
D.-G. Yoo
C.-W. Lee
E.-I. Lee
机构：
[1] Department of Oceanography,
[2] Chungnam National University,undefined
[3] Taejon 305-764,undefined
[4] Korea e-mail: scpark@cnu.ac.kr,undefined
[5] Korea Institute of Geology,undefined
[6] Mining and Materials,undefined
[7] Taejon 305-350,undefined
[8] Korea,undefined
来源：
Geo-Marine Letters | 2000年 / 20卷
关键词：
Japan; Distribution Pattern; Glacial Period; Radiocarbon Date; Warm Tsushima Current;
D O I：
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学科分类号：
摘要：
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 presumably continued at that time through the Korea Strait. The activity of the paleo-Tsushima Current is evidenced by the distribution pattern of river-derived lowstand deposits, consisting of a beach/shoreface complex and lowstand deltaic wedges.
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页码：64 / 71
页数：7
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