Zobrazeno 1 - 10
of 33
pro vyhledávání: '"沖積層"'
Publikováno v:
帝京科学大学紀要 = Bulletin of Teikyo University of Science. 19:49-57
Publikováno v:
帝京科学大学紀要 = Bulletin of Teikyo University of Science. 19:149-159
Publikováno v:
帝京科学大学紀要 = Bulletin of Teikyo University of Science. 18:41-46
Publikováno v:
科学研究費助成事業 研究成果報告書. :1-4
研究成果の概要 (和文) : 濃尾平野内陸域の沖積層の解析・分析に基づいて、完新世の堆積過程を検討した。2本のオールコア堆積物は、現氾濫原のプロデルタ堆積物が分布しない地域で採
Publikováno v:
近畿大学教育論叢 = The Research Journal of the Department of Teacher Education Kindai University. 29(1):43-58
Autor:
Oka, Takao, Kondo, Tsutomu, Nakamura, Toshio, Yasui, Satoshi, Hoshino, Fusa, Yonemichi, Hiroshi, Yamazaki, Yoshiki, Sekine, Tatsuo, Wakamatsu, Mikio, Akamatsu, Shuhei, Inui, Tetsuya
Publikováno v:
名古屋大学年代測定研究. 1:78-84
We performed AMS14C-dating of twelve samples from the basin of Azuma River including HAP-1 and AKP-1 core samples, which were not 14C-measured in 2015 due to machine trouble with the Tandetron AMS system at Nagoya University. The sedimentary water co
Publikováno v:
都市防災研究論文集. 3:19-24
これまでに大阪・神戸地域を対象に, 沖積層(As, Ma13)及び上部洪積層(Dg1, Ma12)の地盤特性をモデル化した「250mメッシュ地盤モデル」を構築した。これを基にして地震時の地表面の揺れやす
Autor:
Oka, Takao, Nakamura, Toshio, Kondo, Tsutomu, Hoshino, Fussa, Yasui, Satoshi, Sekine, Tatsuo, Yonemichi, Hiroshi, Yamazaki, Yoshiki, Wakamatsu, Mikio, Maeda, Toshitsugu, Inui, Tetsuya, Nara, Tomonori
Publikováno v:
名古屋大学加速器質量分析計業績報告書. 27:61-66
The authors have been studied deposits of Late Pleistocene to Holocene in the basin of the Azuma River since spring in 2013 by the use drilling cores. In the year of 2015 they obtained two cores (HAP-1 and AKP-1) by hand-operated sampler, and investi
Publikováno v:
都市防災研究論文集. 2:13-18
これまでに大阪地域の沖積層の250mメッシュモデルを構築したが, 地震時の揺れやすさ評価の基となる工学的基盤は, 十分硬く, 地震動の特性が同じと見なせる必要がある. そこで, 沖積層
Autor:
Oka, Takao, Yasui, Satoshi, Kondo, Tsutomu, Hoshino, Fusa, Nakamura, Toshio, Sekine, Tatsuo, Yonemichi, Hiroshi, Yamazaki, Yoshiki, Inui, Tetsuya, Nara, Tomonori, Shukuda, Koji, Wakamatsu, Mikio, Kusaka, Hajime
Publikováno v:
名古屋大学加速器質量分析計業績報告書. 26:67-72
Five drilling cores (AZK-101, AZK-2, AZK-3, AZK-4 and AZK-5) in the area Hamaatsuma to Kamiatsuma and four hand-operated drilling peat cores in the area Tomisato to Poronai along Azuma River, southern Hokkaido, were investigated based on lithologic o