Japan Geoscience Union Meeting 2016

Presentation information


Symbol O (Public) » Public

[O-02] Poster presentations by senior high school students

Sun. May 22, 2016 1:45 PM - 3:15 PM Poster Hall (International Exhibition Hall HALL6)

Convener:*Tatsuhiko Hara(International Institute of Seismology and Earthquake Engineering, Building Research Institute), Miwa Kuri(International Research Institute of Disaster Science, Tohoku University), Keiko Konya(Research Institute for Global Change, Japan Agency for Marine-Earth Science and Technology), Hajime Naruse(Department of Geology and Mineralogy, Graduate School of Science, Kyoto University), Kou Yamada(Waseda University)

1:45 PM - 3:15 PM

[O02-P58] Sedimentary environment of the Nabeyama Formation in the Kuzu district

*Hidetoshi Masuda1, Naoki Iwamoto1 (1.Kaijo senior high school)

Keywords:Limestone, Sedimentary environment

The Nabeyama Formation consist of Permian carbonate rocks and distribute in the Kuzu district, Sano, Tochigi. This Formation is divisible into the lower part, the middle part, and the upper part (Yanagimoto, 1973). The lower part limestone include fossil of plants, debris of shells, crinoids, bryozoans and so on. Therefore, it is very probable that allochthonous was brought by some factors such as storm. Most of the middle part was changed into dolostone from limestone, so, there is no structure or fossil that indicate environment. The upper part limestone is mainly consist of a lot of fusulinas, it probably means its sedimentary environment is different from this of lower part.