Zhu Li-ping | Institute Of Tibetan Plateau Research Chinese Academy Of Sciences
スポンサーリンク
概要
関連著者
-
Zhu Li-ping
Institute Of Tibetan Plateau Research Chinese Academy Of Sciences
-
Feng Jin-liang
Institute Of Tibetan Plateau Research Chinese Academy Of Sciences
-
Feng Jin‐liang
Inst. Tibetan Plateau Res. Chinese Acad. Sci. Beijing Chn
-
Zhu Li‐ping
Inst. Tibetan Plateau Res. Chinese Acad. Sci. Beijing Chn
-
Zhen Xiao-lin
Institute Of Tibetan Plateau Research Chinese Academy Of Sciences
-
Gao Shao-peng
Institute Of Tibetan Plateau Research Chinese Academy Of Sciences
-
Wu Guang-jian
Institute Of Tibetan Plateau Research Chinese Academy Of Sciences
-
Xia Zhong-huan
Institute Of Tibetan Plateau Research Chinese Academy Of Sciences
-
Sachse D.
Max-planck-institute For Biogeochemistry
-
Xu Bai-qing
Institute Of Tibetan Plateau Research Chinese Academy Of Sciences
-
HU ZHAO-GUO
Institute of Tibetan Plateau Research, Chinese Academy of Sciences
-
JU JIAN-TING
Institute of Geographical Sciences and Nature Resources Research, Chinese Academy of Sciences
-
ZHOU LI-PING
Department of Geography, Peking University
-
ZHANG WEN
Institute of Atmospheric Physics, Chinese Academy of Sciences
-
Hu Zhao-guo
Institute Of Tibetan Plateau Research Chinese Academy Of Sciences
-
Ju Jian-ting
Institute Of Geographical Sciences And Nature Resources Research Chinese Academy Of Sciences
-
CUI ZHI-JIU
Department of Geography, Peking University
-
MUGLER I.
Max-Planck-Institute for Biogeochemistry
-
GLEIXNER G.
Max-Planck-Institute for Biogeochemistry
-
Cui Zhi-jiu
Department Of Geography Peking University
-
Zhang Wen
Institute Of Atmospheric Physics Chinese Academy Of Sciences
著作論文
- Grain size effect on Sr and Nd isotopic compositions in eolian dust : Implications for tracing dust provenance and Nd model age
- Heavy dust fall in Beijing, on April 16-17, 2006 : Geochemical properties and indications of the dust provenance
- Origin of terra rossa over dolomite on the Yunnan-Guizhou Plateau, China
- Hydrogen isotope ratios of terrigenous n-alkanes in lacustrine surface sediment of the Tibetan Plateau record the precipitation signal