Zobrazeno 1 - 10
of 38
pro vyhledávání: '"Oka, Takao"'
Autor:
Oka, Takao, Hoshino, Fusa, Minami, Masayo, Nakamura, Toshio, Wakamatsu, Mikio, Kondo, Tsutomu, Sekine, Tatsuo, Yonemichi, Hiroshi
Publikováno v:
名古屋大学年代測定研究. 5:23-29
北海道中央部の2地域(千歳川水系舞鶴遊水地・手稲山山麓滝の沢川沿い)で湿原堆積物について、地表から2m以内において試料採取を行い、花粉分析とAMS14C年代を実施した。その結果、
Autor:
Hoshino, Fusa, Oka, Takao, Haruki, Masahiro, Nakamura, Toshio, Minami, Masayo, Kondo, Tsutomu, Yonemichi, Hiroshi, Sekine, Tatsuo, Yamazaki, Yoshiki, Wakamatsu, Mikio
Publikováno v:
名古屋大学年代測定研究. 4:16-26
The authors conducted pollen analysis on 35 samples collected from No.1 core of Lake Akan and on 100 samples from No.1 core of Toyozumi, Lake Abashiri and also performed AMS 14C dating on 6 samples from the area, where vegetation changes have been co
Publikováno v:
名古屋大学年代測定研究. 3:11-22
The Society for study of Alluvial plain in the Ishikari depression (SSAI) continued researching into topography and Quaternary geology of basin of Azuma River in Atsuma Town, south part of central Hokkaido, since 2012. On September 6 in 2018, Hokkaid
Autor:
Oka, Takao, Hoshino, Fusa, Nakamura, Toshio, Akamatsu, Shuhei, Kondo, Tsutomu, Yonemichi, Hiroshi, Sekine, Tatsuo, Yamazaki, Yoshiki, Wakamatsu, Mikio
Publikováno v:
名古屋大学年代測定研究. 3:23-30
The Iwanai Plain lies on the coast of Sea of Japan, southwestern Hokkaido. The authors have researched two boring cores (IWS-1 and IWS-2) in Sokonai branch of Horikappu River by means of lithological analysis, AMS14C-dating, and pollen analysis, and
Autor:
Hoshino, Fusa, Oka, Takao, Nakamura, Toshio, Akamatu, Syuhei, Kondo, Tsutomu, Yonemichi, Hiroshi, Sekine, Tatsuo, Yamazaki, Yoshiki, Wakamatsu, Mikio
Publikováno v:
名古屋大学年代測定研究. 3:31-40
To investigate vegetational change in Upper Pleistocene to Holocene temporal range, lithological analysis, AMS 14C-dating and pollen analysis are conducted for the two cores (SMF-1 and SMF-2) drilled at the southeast side of Maeda Forest Park in the
Publikováno v:
名古屋大学年代測定研究. 2:18-23
Authors studied the surface environmental change of the Apporo Dam area in the upper stream of Azuma River, Central Hokkaido since 60 ka by methods of the classification of geomorphic surface, AMS14C dating and pollen analysis. Six terrace surfaces (
Autor:
Sekine, Tatsuo, Nakamura, Toshio, Hoshino, Fusa, Maeda, Hisatsugu, Oka, Takao, Kondou, Tsutomu, Yonemichi, Hiroshi, Yamazaki, Yoshiki, Akamatsu, Shuuhei, Wakamatsu, Mikio
Publikováno v:
名古屋大学年代測定研究. 1:92-97
We, the members of a group studying the Ishikari alluvial plain, are investigating the paleoenvironment of the layer in the Quaternary period of the Atsuma area. We obtained a drilling core from the Teine area on the Sea of Japan side in 2015 and hav
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
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