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Reply to comments by H. Mashima on ‘Evolution of the eastern margin of Korea: constraints on the opening of the East Sea (Japan Sea)’ by Kim et al. [Tectonophysics 436 (2007) 37–55]
Authors:Han-Joon Kim  Gwang Hoon Lee  Hyeong-Tae Jou
Institution:aMarine Environment & Characteristics, Korea Ocean R & D Institute, Ansan P.O. Box 29, 425-600, Korea;bDept. of Environmental Exploration Engineering, Pukyong National University, Busan 608-737, Korea
Abstract:We thank H. Mashima for his interest in our recent article in Tectonophysics Kim, H.J., Lee, G.H., Jou, H.T., Cho, H.M., Yoo, H.S., Park, G.T., Kim, J.S., 2007, Evolution of the eastern margin of Korea: Constraints on the opening of the East Sea (Japan Sea). Tectonophysics 436, 37–55.] and welcome the opportunity to respond to his comments. In our article we suggested that the southern part of the East Sea (Japan Sea) opened principally in the southeast direction in response to the northwestward subduction of the Pacific Plate beneath the Japan Arc. In contrast, Mashima claims that the opening of the East Sea was achieved in the south–southeast direction. However, there are many crucial things in his comments that we find scientifically unconvincing and misleading. In this reply, we give a detailed response to his comments.
Keywords:East Sea  Korean margin  Separation of SW Japan  Yamato Bank  Korea Plateau
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