The Kamuikotan Tectonic Belt in Hokkaido, Japan, was Probably Formed as a Strike-Slip Mobile Zone Associated with Oblique Subduction and Obduction Processes during Mesozoic Time (abs.)

Authors=ISHIZUKA Hideo, IMAIZUMI Masayuki, GOUCHI Nobuo

Journal/Book_names=Oji International Seminar on Accretion Tectonics

pages=29-29

Publish_year=1981

Publish_Country=JPN

Publisher=Japan Society of the Promotion of Science, Fujihara Foundation of Science

Language_of_Text=EN

ID=201512267