Characteristics of the late Quaternary tephra layers in the East/Japan Sea and their new occurrences in western Ulleung Basin sediments-Reference-Cited by-同舟云学术

Characteristics of the late Quaternary tephra layers in the East/Japan Sea and their new occurrences in western Ulleung Basin sediments

Published:2003-11 Issue:3-4 Volume:202 Page:135-142
ISSN:0025-3227
Container-title:Marine Geology
language:en
Short-container-title:Marine Geology

Author:

Park Myong-Ho,Kim Il-Soo,Shin Jae-Bong

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology,Oceanography

Reference23 articles.

1. Characteristics of the Late Pleistocene marker-tephras of South Kanto, Central Japan;Arai;Quat. Res.,1977

2. Late Quaternary tephrochronology and paleo-oceanography of the sediments of the Japan Sea;Arai;Quat. Res. Japan,1981

3. Origins and paleoceanographic significance of laminated muds from the Ulleung Basin, East Sea (Sea of Japan);Bahk;Mar. Geol.,2000

4. Sedimentary records of paleoenvironmental changes during the last deglaciation in the Ulleung Interplain Gap, East Sea (Sea of Japan);Bahk;Glob. Planet. Change,2001

5. Chough, S.K., 1982. Turbidites in the Ulleung (Tsushima) back-arc basin, East Sea (Sea of Japan). In: Hoshino, M., Shibasaki, T. (Eds.), Geology of Japan Sea. Tokai Univ. Press, Tokyo, pp. 365–376.

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