Zobrazeno 1 - 6
of 6
pro vyhledávání: '"鬼界アカホヤ火山灰"'
Publikováno v:
宮崎県埋蔵文化財センター研究紀要 : 宮崎県埋蔵文化財センター研究紀要第8集. 8:92-102
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=jairo_______::00ea3c77dff478720b9874d6845830dd
http://sitereports.nabunken.go.jp/article/120236
http://sitereports.nabunken.go.jp/article/120236
Autor:
Shiba, Kojiro
2014～2017年度日本学術振興会科学研究費助成事業（学術研究助成基金助成金）（若手研究（B））課題番号（26770278）
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=jairo_______::7d2fed8c7795b2a8ab5c7211bc090274
http://hdl.handle.net/11177/6697
http://hdl.handle.net/11177/6697
Publikováno v:
日本海域研究 = Japan sea research. 45:63-74
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=jairo_______::4a46ca84bfb8fb9a775d928a794fc1e0
http://hdl.handle.net/2297/37023
http://hdl.handle.net/2297/37023
Publikováno v:
地学雑誌. 111(5):661-683
The Median Tectonic Line (MTL) active fault system is one of the most active intraplate faults in Japan. The fault system, which is more than 300 km long, is a right-lateral strike-slip fault with an average slip rate of 5-10 mm/y in east Shikoku. Th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=jairo_______::61f5733d9078fffa70cdc8a7f2c45f1f
http://repo.lib.tokushima-u.ac.jp/117634
http://repo.lib.tokushima-u.ac.jp/117634
Publikováno v:
広島大学学校教育学部紀要. 第二部. 22:15-20
K-Ah volcanic ash and volcanic glasses derived from Aira-Tn volcanic ash were discovered from terrace deposits on the bank of Miharagawa river in Sera-Nishi Town. The terrace deposits are lithologically divided into the A and B formations in ascendin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::a76386d688000f0e909038f012025e17
http://ir.lib.hiroshima-u.ac.jp/00027372
http://ir.lib.hiroshima-u.ac.jp/00027372
Publikováno v:
広島大学学校教育学部紀要. 第二部. 22:15-20
K-Ah volcanic ash and volcanic glasses derived from Aira-Tn volcanic ash were discovered from terrace deposits on the bank of Miharagawa river in Sera-Nishi Town. The terrace deposits are lithologically divided into the A and B formations in ascendin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=jairo_______::bd1ba8ebdac3f0bedafa2d870fb1c1f4
https://ir.lib.hiroshima-u.ac.jp/00027372
https://ir.lib.hiroshima-u.ac.jp/00027372