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GE Quansheng~1 WANG Shaowu~2 WEN Xinyu~2 Caiming SHEN~3 HAO Zhixin~(*1) 1 Institute of Geographical Sciences and Natural Resources Research,Chinese Academy of Sciences,Beijing 100101 2 Department of Atmospheric Science,School of Physics,Peking University,Beijing 100871 3 Atmospheric Sciences Research Center,State University of New York,Albany,New York 12203,USA;Temperature and Precipitation Changes in China During the Holocene[J];大气科学进展(英文版);2007-06 |
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Bruce Denness(Bureau of Applied Sciences Wydcombe Manor, Whitwell, I. W., P038 2NY, England);THE VARIATION OF THE UNIVERSAL GRAVITATIONAL CONSTANT AND THE DISTRIBUTION OF EARTHQUAKES IN CHINA THROUGH TIME AND SPACE[J];Seismology and Geology;1989-02 |
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WANG Yong1,2,3, SHEN Ji1*, XU Xingna1,4, LIU Xingqi1, SIROCKO Frank3, ZHANG Enlou1, and JI Junfeng5 1 State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Nanjing 210008, China 2 Max Planck Institute of Chemistry, Mainz 55020, Germany 3 Institute of Geoscience, University of Mainz, Mainz 55099, Germany 4 School of Geographical Science, Southwest University, Chongqing 400715, China 5 Department of Earth Sciences, Nanjing University, Nanjing 210093, China;Environmental changes during the past 13500 cal. a BP deduced from lacustrine sediment records of Lake Qinghai, China[J];中国地球化学学报(英文版);2011-04 |
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SHI Yafeng YAO Tandong
(Lanzhou Institute of Glaciology and Geocryology, Chinese Academy of Sciences, Lanzhou 730000, China)
YANG Bao
(Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, China);Decadal climatic variations recorded in Guliya ice core and comparison with the historical documentary data from East China during the last 2000 years[J];中国科学(D辑:地球科学)(英文版);1999-S1 |
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CHEN Fahu, ZHU Van, LI Jijun, SHI Qi, JIN Liya & B. WunemannNational Laboratory of Western China's Environmental Systems, Lanzhou University, Lanzhou 730000, China;College of Geography and Environmental Science, Northwest Normal University, Lanzhou 730070, China;South China Sea Institute of Oceanography, Chinese Academy of Sciences, Guangzhou 510301, China;Institute of Geographical Science, Department of Geosciences, Free University of Berlin, 12249 Berlin, Germany;Abrupt Holocene changes of the Asian monsoon at millen- nial- and centennial-scales: Evidence from lake sediment document in Minqin Basin, NW China[J];科学通报(英文版);2001-23 |
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JIN Zhangdong1, 2, WANG Sumin1, SHEN Ji1 & WANG Yinxi 3 1. Key Laboratory of Lake Sedimentation and Environment, Nanjing Institute of Geography & Limnology, Chinese Academy of Sciences, Nanjing 210008, China; 2. State Key Laboratory for Research of Mineral Deposits, Nanjing University, Nanjing 210093, China; 3. Center of Materials Analysis, Nanjing University, Nanjing 210093, China Correspondence should be addressed to Jin Zhangdong (e-mail: zhdjin@niglas.ac.cn);Carbonate verse silicate Sr isotope in lake sediments and its response to Little Ice Age[J];科学通报(英文版);2003-01 |
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LI DongLing 1,JIANG Hui 1,LI TieGang 2 & ZHAO MeiXun 3 1 Key Laboratory of Geographic Information Science,East China Normal University,Shanghai 200062,China;2 Key Laboratory of Marine Geology and Environment,Institute of Oceanology,Chinese Academy of Sciences,Qingdao 266071,China;3 Key Laboratory of Theoretical and Applied Marine Chemistry and Chemical Engineering of the Ministry of Education,Ocean University of China,Qingdao 266100,China;Late Holocene paleoenvironmental changes in the southern Okinawa Trough inferred from a diatom record[J];科学通报(英文版);2011-11 |
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Zhang Qingsong
Institute of Geography, Chinese Academy of Sciences, Beijing 100101;EVOLUTION OF THE ANTARCTIC ICE SHEET SINCE LATE PLEISTOCENE[J];南极研究(英文版);1990-00 |
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;Dark Ages Cold Period[J];Advances in Climate Change Research;2011-03 |
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LIU Shengfa 1,2,SHI Xuefa 1,2 ,LIU Yanguang 1,2,WU Yonghua 1,2,YANG Gang 1,2 1 First Institute of Oceanography,State Oceanic Administration,Qingdao 266061,China 2 Key Laboratory of Marine Sedimentology and Environmental Geology,State Oceanic Administration,Qingdao 266061,China;Environmental record from the mud area on the inner continental shelf of the East China Sea since the mid-Holocene[J];海洋学报(英文版);2011-04 |
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