A broad distribution of accreted intraplate volcanic edifice in the Late Cretaceous Tokoro greenstone belt, NE-most of Japan


Shunta Sakai1, Naoto Hirano2, Yildirim Dilek3, Shiki Machida4,5, Kazutaka Yasukawa4,6 and Yasuhiro Kato4,6, (1)Tohoku University, Graduate school of science, Sendai, Japan, (2)Tohoku University, Center for Northeast Asian Studies, Sendai, Japan, (3)Miami University Oxford, Geology & Environmental Earth Science, Oxford, OH, United States, (4)Chiba Institute of Technology, Ocean Resources Research Center for Next Generation, Chiba, Japan, (5)The University of Tokyo, Department of Systems Innovation, School of Engineering, Tokyo, Japan, (6)The University of Tokyo, Tokyo, Japan