Comparative analysis of BDS-T1 tephra from Baekdusan volcano and Middle Pleistocene B-KY1 tephra from marine core in the East Sea

Author:

Chun Jong-Hwa,Cheong Daekyo

Funder

Korea Institute of Geoscience and Mineral Resources

Publisher

The Geological Society of Korea

Subject

Earth and Planetary Sciences (miscellaneous),Geology

Reference17 articles.

1. Recurrent Quaternary magma generation at Baekdusan (Changbaishan) volcano: New zircon U-Th ages and Hf isotopic constraints from the Millennium Eruption

2. Reconstruction of the history of Plinian eruptions using the marine tephrostratigraphy of volcanoes around the East Sea, Korea

3. Origin of Compositional Diversity of Marine Tephra during the Late Middle Pleistocene B-KY1 Baekdusan Volcanic Eruption

4. Chun, J.-H., Cheong, D., Han, S.-J., Huh, S. and Yoo, H.-S., 2006a, Tephrostratigraphy and paleoenvironments of marine core in the Kita-Yamato Trough, East Sea/Japan Sea. Economic and Environmental Geology, 39, 83-93 (in Korean with English abstract).

5. Chun, J.-H., Cheong, D., Lee, Y.-J., Kwon, Y.-I. and Kim, B.-C., 2006b, Stratigraphic implications as a time marker of the B-J tephra erupted from Baegdusan volcano discovered in the marine cores of the East Sea/Japan Sea during the late Pleistocene. Journal of the Geological Society of Korea, 42, 31-42 (in Korean with English abstract).

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