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| 1 |
Qin Xiaoguang Cai Binggui Liu Tungsheng (Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029);CHARACTERISTICS OF ATMOSPHERIC TURBULENCE IN THE EASTERN ASIAN MONSOON AREA DURING MIS 3[A];[C];2003 |
| 2 |
AO Hong~(1,2) 1 Paleomagnetism and Geochronology Laboratory(SKL-LE),Institute of Geology and Geophysics, Chinese Academy of Sciences,Beijing 100029,China 2 Graduate University of Chinese Academy of Sciences,Beijing 100049,China;Rock magnetic properties of the fluvio-lacustrine sediments from the Dachangliang section in the Nihewan Basin,northern China[A];[C];2009 |
| 3 |
HUANG Lei ZHANG Yunxiang GONG Hujun (Key Laboratory of Continental Dynamics of the Ministry of Education and Department of Geology,Northwest University,Xi'an 710069,Shaanxi);GENESIS OF NEOGENE“RED CLAY”IN LINXIA BASIN,GANSU PROVINCE AND ITS GEOLOGICAL SIGNIFICANCES[A];[C];2004 |
| 4 |
WEI Jianjing~1 & GUO Zhengtang~(2,1) 1.Institute of Geology and Geophysics,Chinese Academy of Sciences, Beijing 100029,China; 2.State Key Laboratory of Loess and Quaternary Geology.Institute of Earth Environment.Chinese Academy of Sciences.Xi'an 710075. China;Changes in the content of eolian iron during the past 900 ka and the implications[A];[C];2003 |
| 5 |
Z.T.Guo~1,B.Sun~(1,2),Z.S.Zhang~(1,3),S.Z.Peng~1,G.Q.Xiao~4,J.Y.Ge~4,Q.Z.Hao~1,Y.S.Qiao~1,M.Y.Liang~1, J.F.Liu~1,Q.Z.Yin~1,and J.J.Wei~1 1 Key Laboratory of Cenozoic Geology and Environment,Institute of Geology and Geophysics,Chinese Academy of Sciences,P.O.Box 9825,Beijing,100029,China 2 Shandong Institute and Laboratory of Geological Sciences,Jinan,250013,China 3 Nansen-Zhu International Research Center,Institute of Atmospheric Physics,Chinese Academy of Sciences,Beijing, 100029,China 4 State Key Laboratory of Loess and Quaternary Geology,Institute of Earth Environment,Chinese Academy of Sciences,P.O. Box 17,Xian,710075,China;A major reorganization of Asian climate by the early Miocene[A];[C];2009 |
| 6 |
Feng Shaohua~(①②) Tang Zihua~①Wang Xu~①Yang Shiling~①(①Key Laboratory of Cenozoic Geology and Environment,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029;②Graduate University of Chinese Academy of Sciences,Beijing 100049);ORIGIN AND AGE OF'RED CLAY'SEDIMENT AT JUNGAR BANNER,INNER MONGOLIA,AND ITS PALAEOCLIMATIC IMPLICATIONS[A];[C];2011 |
| 7 |
Qingzhen Hao~(a,*),Zhengtang Guo~a,Yansong Qiao~(b,c),Bing Xu~a,Frank Oldfield~d a Key Laboratory of Cenozoic Geology and Environment,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China b Institute of Geomechanics,Chinese Academy of Geological Sciences,Beijing 100081,China c Key Laboratory of Neotectonic Movement & Geohazard,Beijing 100081,China d School of Environmental Sciences,University of Liverpool,Liverpool,L69 7ZT,UK;Geochemical evidence for the provenance of middle Pleistocene loess deposits in southern China[A];[C];2011 |
| 8 |
ZHAO XiangYu~(1,2) & LIU QingSong~(1*) 1 Paleomagnetism and Geochronology Laboratory(SKL-LE),Institute of Geology and Geophysics,Chinese Academy of Sciences, Beijing 100029,China; 2 Graduate University of Chinese Academy of Sciences,Beijing 100049,China;Effects of the grain size distribution on the temperature-dependent magnetic susceptibility of magnetite nanopartieles[A];[C];2011 |
| 9 |
Liu Xianbin Xia Dunsheng Jia Jia;Magnetic properties and its signification to palaeoclimate by Jiuzhoutai loess in Lanzhou[A];[C];2011 |
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