文献
J-GLOBAL ID:201702246150626340
整理番号:17A0204888
洞窟生成物の酸素同位体記録はモンスーン降雨量変動を反映する完新世は期間中の東アジア夏季モンスーン最大のタイミングについて【Powered by NICT】
On the timing of the East Asian summer monsoon maximum during the Holocene-Does the speleothem oxygen isotope record reflect monsoon rainfall variability?
著者 (9件):
Chen Jianhui
(College of Earth and Environmental Sciences, Lanzhou University)
,
Rao Zhiguo
(College of Earth and Environmental Sciences, Lanzhou University)
,
Liu Jianbao
(College of Earth and Environmental Sciences, Lanzhou University)
,
Huang Wei
(College of Earth and Environmental Sciences, Lanzhou University)
,
Feng Song
(Department of Geosciences, University of Arkansas)
,
Dong Guanghui
(College of Earth and Environmental Sciences, Lanzhou University)
,
Hu Yu
(College of Earth and Environmental Sciences, Lanzhou University)
,
Xu Qinghai
(Institute of Nihewan Archaeology Research, Hebei Normal University)
,
Chen Fahu
(College of Earth and Environmental Sciences, Lanzhou University)
資料名:
Science China. Earth Sciences
(Science China. Earth Sciences)
巻:
59
号:
12
ページ:
2328-2338
発行年:
2016年
JST資料番号:
C2577A
ISSN:
1674-7313
資料種別:
逐次刊行物 (A)
記事区分:
原著論文
発行国:
中国 (CHN)
言語:
英語 (EN)