Collision between the Izu and Honshu Arcs and strike-slip deformation along the Tanna Fault Zone: northward motion of the northeastern block in the Izu Peninsula, estimated by deformation rate detected by paleomagnetism(poster session)(abs.)

Authors=KIMURA Haruo

Journal/Book_names=Proceedings of the 1st Annual Meeting of the Kanto Branch, Geological Society of Japan"Geology in the Kanto District"

pages=37-39

Publish_year=2007

Publish_Country=JPN

Publisher=Kanto Branch, Geological Society of Japan

Language_of_Text=JA

ISSN=09173404

ID=200922421