@article{oai:nagoya.repo.nii.ac.jp:00012784,
 author = {齊藤, 毅 and SAITO, Takeshi and 星野, 光雄 and HOSHINO, Mitsuo and 束田, 和弘 and TSUKADA, Kazuhiro and 中村, 俊夫 and NAKAMURA, Toshio and 桂田, 祐介 and KATSURADA, Yusuke and 田中, 剛 and TANAKA, Tsuyoshi and 吉田, 英一 and YOSHIDA, Hidekazu},
 journal = {名古屋大学博物館報告},
 month = {Dec},
 note = {River terraces around Tell Ghanem al-Ali, Raqqa, Syria, were studied to clarify geological and environmental settings of the tell. Five levels of terraces are recognizable on the basis of available topographic maps and field observation: terraces I (250 m a.s.l.), II (242–245 m), III (237–240 m), IV (233–234 m) and V (ca. 230 m) in descending order. Tell Ghanem al-Ali is located on the terrace V (lowermost terrace), which is 1–2 m higher than the flood plain of Euphrates. Sediments around the tell are divided into five units: channel and flood plain deposits of modern Euphrates, sediments of the lowermost terrace and Units 1–3. Stratigraphic relationship among them suggests that Unit 1, Unit 2 and sediment of the lowermost terrace were deposited in the depositional phase of this area, and that terraces I–IV were formed in the erosional phase. Stratigraphy of the Tell Ghanem al-Ali and the lowermost terrace, and available 14C dating data indicate that settlement of the tell began during the formation of the lowermost terrace at ca. 3000 cal y BC.},
 pages = {13--20},
 title = {シリア・ラッカ県，Tell Ghanem al-Ali 周辺に発達する河成段丘},
 volume = {26},
 year = {2010}
}