@article{oai:kumadai.repo.nii.ac.jp:00029724,
 author = {Tsuru, Arisa and Takashima, Shiori and 高嶌, 栞織 and Tanaka, Hitoshi and 津留, ありさ and Takashima, Shiori and 高嶌, 栞織 and 田中, 均},
 journal = {熊本大学教育学部紀要},
 month = {Dec},
 note = {application/pdf, 論文(Article), The Saitsu Formation, which is distributed in the Amakusa area of Kumamoto Prefecture and rests unconformably upon the Middle Miocene Sakasegawa Formation, has been considered to range 3.0±0.3 Ma by fission track method. The formation is divided into the lower and upper members based on the Goryou Pyroclastic Frow Deposits.
The Saitsu Formation is characterized by conglomerate, sandstone, mudstone, ofen tuffaceous shale. The upper half of upper member is mainly composed of tuffeceous sand, tuffite with thin interbeds of tuffaceous mudstone. The conglomerate is moderately sorted, comprising subrounded to rounded boulders and cobbles of chart, granitic rocks,
schist and volcanic rocks. The chart, schist and granitic rocks which constitute conglomerate are not distributed the Amakusa area. It is one of the purposes of this reserch where those stones have been carried out how and when from and to solve. The result of investigation showed that activity of the Futagawa Fault was greatly involving about constitute of the Saitsu Formation containing many conglomerate. Furthermore, it turned out that a chart, schist, and granites have been carried from the Chichibu and Higo Belts located in central Kumamoto, respectively. On the other hand, while the teaching-materials these results of an investigation for the junior high school student, it tied to lesson practice.},
 pages = {255--263},
 title = {天草に位置する佐伊津層の教材化と授業実践},
 volume = {65},
 year = {2016},
 yomi = {タカシマ, シオリ and タカシマ, シオリ and タナカ, ヒトシ}
}