Abstract
Terrace stratigraphy of the southeastern coastal areas of Korea has been studied with the help of terrace mapping and geochronology. Coastal terraces include 90–130 m upper High Terrace (uHT), 63–86 m High Terrace (HT), 36–55 m Middle Terrace (MT) and 8–25 m Low Terrace (LT) divisions, each of which has been subdivided. Amongst these, LT 2 formed during the late Pleistocene, based on Tephras Aso-4 (MIS 5c), Ata (MIS 5d or 5e) and OSL ages. The age of LT 1–3 ranges from MIS 5e to 5a, based on tephra ages from Aso-4 (ca. 90 ka) and Ata (100–125 ka). The uplift rate in the SE part of Korea ranges between 0.14 and 0.22 mm/a and it is quite small in comparison to the Japanese island arc, or many other tectonically active East and Southeastern Asian regions.
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