Micropaleontological and seismic observations for early developmental stage of the southwestern Ulleung Basin, East Sea (Japan Sea)

The Ulleung Basin is located in the southwestern part of the East Sea (Japan Sea) and contains thick Neogene sediment. Detailed examination of the stratigraphic distribution of dinoflagellates was carried out on samples from the onshore Pohang Basin (E well) and two wells (Gorae I and Dolgorae VII)...

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Bibliographic Details
Published in:The island arc Vol. 16; no. 2; pp. 262 - 275
Main Authors: Yun, Hyesu, Yi, Songsuk, Oh, Jinyong, Byun, Hyunsook, Shin, Kooksun
Format: Journal Article
Language:English
Published: Melbourne, Australia Blackwell Publishing Asia 01-06-2007
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Summary:The Ulleung Basin is located in the southwestern part of the East Sea (Japan Sea) and contains thick Neogene sediment. Detailed examination of the stratigraphic distribution of dinoflagellates was carried out on samples from the onshore Pohang Basin (E well) and two wells (Gorae I and Dolgorae VII) in the southwestern Ulleung Basin, to investigate the early evolution of the basin. The results show that thick syn‐rift sediments mainly consist of terrestrial deposits and are widespread over the basin. This supports an extensional tectonic origin for the basin. The initiation of the deposits dates back to 17–16.4 Ma. Furthermore, well‐preserved Eocene to Oligocene dinoflagellate taxa found in Miocene deposits of wells implies that the age of initial rifting might be Oligocene or earlier. Our results provide constraints for understanding the opening process of the East Sea.
Bibliography:ark:/67375/WNG-R0BZRG0V-2
ArticleID:IAR571
istex:16AC19D6ACFBEEC9203281206B3FE24B9A2FFF92
ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
ISSN:1038-4871
1440-1738
DOI:10.1111/j.1440-1738.2007.00571.x