@article{oai:tokyo-metro-u.repo.nii.ac.jp:00002977,
 author = {クワバラ, タクイチロウ and Kuwabara, Takuichiro},
 issue = {36},
 journal = {Geographical Reports of Tokyo Metropolitan University},
 month = {},
 note = {In the Kamikita Plain of the "mid-lowland" of the northeast Japan arc, the marine Pleistocene sediment "Noheji formation" consists of the basements under marine terraces as revealed by previous studies. The Noheji formation is rather thick as if this formation had accumulated in a subsiding basin. The geomorphologic and geological structures, however, reveal that the Noheji formation is an assemblage of marine-terrace deposits newly recognized in the Kamikita Plain. Because marine terraces and their deposits are generally formed by the glacial eustacy in uplifted regions, the Kamikita Plain has been uplifting on and after the accumulation of the Noheji formation. This formation didn't occur in the subsiding region, but built up with the glacial eustacy in the uplifted Kamikita Plain.},
 pages = {17--28},
 title = {Quaternary tectonic movement deduced from marine terraces and noheji formation in the kamikita plain, shimokita peninsula, northeast japan},
 year = {2001}
}