@article{oai:nagoya.repo.nii.ac.jp:00015708,
 author = {山本, 直人 and YAMAMOTO, Naoto},
 journal = {名古屋大学文学部研究論集. 史学},
 month = {Mar},
 note = {The Okyoduka type of c. 1300-c. 1100 cal BC and the Nakaya type of c.11OO-c.900 cal BC in the Tedorigawa alluvial fan look like the Kamegaoka type of the Tohoku district because they are greatly influenced by the Kamegaoka type. The shards of Tottaimon type are found during the Shimono type of c.900-c.800 cal BC in the Okyouduka site, and these come from the Tottaimon type of the west part of the Japanese Islands. The shards of Ongagawa type are found during the Nagatake type of c.800-c.600 cal BC and the Shibayama-demura type of c. 600-c. 350 cal BC in the Awata site, the Inui site and the Hattanaka site, and these come from the Ongagawa type of the west part of the Japanese Islands.},
 pages = {61--72},
 title = {縄文晩期の手取川扇状地における外来系土器の移入形態},
 volume = {59},
 year = {2013}
}