@article{oai:ir.soken.ac.jp:00003943,
 author = {那須, 浩郎 and SAWAI, Yuki and SATAKE, Kenji and KAMATAKI, Takanobu and NASU, Hiroo and et, al.},
 issue = {5703},
 journal = {Science, Science},
 month = {Dec},
 note = {In eastern Hokkaido, 60 to 80 kilometers above a subducting oceanic plate, tidal mudflats changed into freshwater forests during the first decades after a 17th-century tsunami. The mudflats gradually rose by a meter, as judged from fossil diatom assemblages. Both the tsunami and the ensuing uplift exceeded any in the region's 200 years of written history, and both resulted from a shallow plate-boundary earthquake of unusually large size along the Kuril subduction zone. This earthquake probably induced more creep farther down the plate boundary than did any of the region's historical events.},
 pages = {1918--1920},
 title = {Transient uplift after a 17th-century earthquake along the kuril subduction zone},
 volume = {306},
 year = {2004}
}