Abstract
The Cretaceous to Paleogene plutonic rocks are widely distributed as a basement rock of the NE Japan Arc. In this report, newly obtained Sr, Nd, Pb, and Hf isotopic composition are reported, and comparison and verification with a geotectonic division and isotope zone division are performed. The epsilon Nd-Sr (0Ma) diagram, the domain of the Abukuma Belt and the Ashio Belt is distinguished clearly. The epsilon Hf-Nd diagram shows the narrow extent, and the Abukuma and the Ashio Belts are distinguished more clearly. Re-classification of isotope zone by Hf isotope may possibly.