Zobrazeno 1 - 10
of 24
pro vyhledávání: '"Yasui, Satoshi"'
Publikováno v:
In Quaternary Science Reviews 2010 29(27):3956-3971
Autor:
Hoshino, Fusa, Nakamura, Toshio, Oka, Takao, Kondo, Tsutomu, Yasui, Satoshi, Yonemichi, Hiroshi, Sekine, Tatsuo, Yamazaki, Yoshiki, Wakamatsu, Mikio, Akamatu, Syuhei
Publikováno v:
名古屋大学年代測定研究. 1:85-91
Pollen analytical studies of the local Atsuma Formation, which consists of Picea and Abies conifers in the late Pleistocene, have indicated a sub-cold climate. AMS14C dating performed in a pollen analytical study of the AZK-101 core revealed 2,000 ye
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:
In Quaternary International 2004 115:117-130
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
Autor:
Hoshino, Fusa, Nakamura, Toshio, Oka, Takao, Kondo, Tsutomu, Sekine, Tatsuo, Yonemichi, Hiroshi, Yamazaki, Yoshiki, Yasui, Satoshi, 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. 27:67-72
The lower part of the AZK-103 core consisted of Picea forest , and the part above it consisted of 86% Sphagnum. Above this, the proportion of Quercus forest decreased gradually. At the lowermost part of the AZK-112 core, coniferous forest material co
Autor:
Yasui, Satoshi, Oka, Takao, Kondo, Tsutomu, Nakamura, Toshio, Hoshino, Fusa, 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. 27:73-78
Four types of diatom assemblage (fresh water, brackish water, marine water and compound assemblage of fresh and marine water species) were detected in alluvial deposits of the Azuma incised-valley area. Environmental changes from late Pleistocene t
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
Autor:
Oka, Takao, Kondou, Tsutomu, Nakamura, Toshio, Hoshino, Fusa, Yasui, Satoshi, Ijima, Yukio, Sekine, Tatsuo, Yonemichi, Hiroshi, Shukuda, Koji, Yamazaki, Yoshiki, Inui, Tetsuya, Nara, Tomonori
Publikováno v:
名古屋大学加速器質量分析計業績報告書. 25:111-124
Two drilling cores (46 meters core of AZK-1 and 25 meters core of S60Kー1), in the lowland along the downstream of Atsuma River, southern Hokkaido, were investigated based on lithologic observation, microbiostratigraphy (pollen and diatom), tephroch