Zonal propagation of kinetic energy and convection in the South China Sea and Indian monsoon regions in boreal summer   总被引：7，自引：0，他引：7  

CHEN Longxun  GAO Hui  HE Jinhai  TAO Shiyan & JIN Zuhui .Chinese Academy of Meteorological Sciences  Beijing  China  .Nanjing Institute of Meteorology  Nanjing  China  .Institute of Atmospheric Physics  Chinese Academy of Sciences  Beijing  China 《中国科学D辑(英文版)》2004,47(12):1076-1084

As early as in the 1980s, Chinese scientists hadfirst proposed that there exits two summer monsoonsystems in Asia, namely the East Asian summer mon-soon (EASM) and the Indian summer monsoon(ISM)[1-4]. The two monsoon systems are quite dif-ferent in characteristics. Since then, such issue andconclusion had been documented and approved by alot of studies in the past two decades, and was appliedin the guideline of the South China Sea summer mon-soon experiment (SCSMEX), which was undertak…  相似文献   

Recent glacial retreat in High Asia in China and its impact on water resource in Northwest China   总被引：48，自引：0，他引：48  

YAO Tandong    WANG Youqing  LIU Shiying    PU Jianchen    SHEN Yongping & LU Anxin  .Institute of Tibetan Plateau Research  Chinese Academy of Sciences  Beijing  China  .Cold  Arid Regions Environmental  Engineering Research Institute  Chinese Academy of Sciences  Lanzhou  China 《中国科学D辑(英文版)》2004,47(12):1065-1075

There are about 46298 glaciers in the High Asiain China, the total glacial area is about 59406 km , andtotal glacial volume about 5590 km3. These glaciersmainly concentrate around the Himalayas Mountains,Nyainqentanglha Mountains, Kunlun Mountains,Karakoram Mountains and Tianshan Mountains. Theglaciers in the Tibetan Plateau are the major compo-nent of the glaciers in the High Asia in China. Theseglaciers extend north to the arid and desert regions,and become the main water resource in …  相似文献   

Geospatial-temporal analysis of land-use changes in the Yellow River Delta during the last 40 years   总被引：5，自引：0，他引：5  

Qinghua?YeEmail author  Gaohuan?Liu  Guoliang?Tian  Shenliang?Chen  Chong?Huang  Shupeng?Chen  Qingshen?Liu  Jun?Chang  Yanan?Shi 《中国科学D辑(英文版)》2004,47(11):1008-1024

Research on land use/land cover changes (LUCC)has been the core project of the Global EnvironmentalChanges since the 1990s[1—6]. Scientists at home andabroad have been laying emphasis on integrationstudies on land-use change by “space and process”features[7—10] as researches on LUCC are in a greatdeal. It is of paramount important for us to studyLUCC at various spatial-temporal scales and build aquantitative assessment of land-use conversion by in-tegrated spatial-temporal features. …  相似文献   

Environmental records of lacustrine sediments in different time scales: Sediment grain size as an example   总被引：2，自引：0，他引：2  

CHEN Jing’an  WAN Guojiang  David Dian Zhang  ZHANG Feng & HUANG Ronggui . State Key Laboratory of Environmental Geochemistry  Institute of Geochemistry  Chinese Academy of Sciences  Guiyang  China  . Department of Geography  Geology  University of Hong Kong  Pokfulam Road  Hong Kong  China 《中国科学D辑(英文版)》2004,47(10):954-960

Understanding the past is the key to know thepresent and to predict the future. As a core project ofthe International Geosphere Biosphere Program, PastGlobal Changes (PAGES) aims to reconstruct theevolution history of global climate, global environ-ment and global ecosystem with resort to all kinds ofnatural records, so as to reveal the change rules(change processes, change amplitude and change rate)of the global environment and thus provide scientificbasis for predicting climate changes p…  相似文献   

Discovery of agglutinated foraminifers from the Longzhaogou Group in eastern Heilongjiang Province   总被引：1，自引：1，他引：0  

LI Gang & YU Shanmao. State Key Laboratory of Paleobiology Stratigraphy  Nanjing Institute of Geology  Paleontology  Chinese Academy of Sciences  Nanjing  China  .th Coal-prospecting Team of Geological Bureau  NE China  Inner Mongolia Coal Company  Jixi  China Correspondence should be addressed to Li Gang 《中国科学D辑(英文版)》2004,47(2):122-127

The low diversity agglutinated foraminifers are recovered from the Qihulin Formation of the Longzhaogou Group in eastern Heilongjiang, China. The foraminiferal fauna consists of 9 species of 5 genera. The common members are Cribrostomoides nonioninoides (Reuss), Haplophragmoides concavus (Chapman), H. gigas minor Nauss. Although the diagnostic zonal taxa are absent in the agglutinated fauna, according to the global stratigraphic distribution of the above-mentioned species, and the associated Pseudohaploceras ammonite fauna, the foraminiferal fauna may be of a Barremian-Aptian (Early Cretaceous) age.  相似文献   

Ore-forming fluid and mineralization of Caijiaying and Dajing polymetallic ore deposits   总被引：3，自引：0，他引：3  

WANG Lijuan  WANG Jingbin  WANG Yuwang & ZHU Heping. Key Laboratory of Mineral Resources  Institute of Geology  Geophysics  Chinese Academy of Sciences  Beijing  China  . Beijing Institute of Geology for Mineral Resources  Beijing  China Correspondence should be addressed to Wang Lijuan 《中国科学D辑(英文版)》2004,47(2):97-107

Fluid inclusions from the Dajing and Caijiaying deposits have nearly the same ho-mogenization temperature. Correlation between temperature and salinity shows that both Sn-and Cu-bearing fluids Sn and Cu were present in the Dajing deposit but only one kind of fluids continuously evolved in the Caijiaying deposit. Study on rare earth elements (REE) in ancient fluid from the inclusions indicates that the fluid of Sn mineralizing stage in Dajing was derived from remelting magma of the continental crust, and the fluid of Cu-Pb-Zn mineralizing stage in the Dajing deposit and the fluid of Cu-Pb-Zn mineralization in the Caijiaying deposit were derived from the mantle. It is concluded that the Cu-Pb-Zn mineralizations in the Dajing and Caijiaying deposits resulted from the identical tectono-thermal event of magma-fluids induced by Mesozoic tectonic transition and extension in the eastern part of North China Craton.  相似文献   

Co-seismic ground deformation and source parameters of Mani M7.9 earthquake inferred from spaceborne D-InSAR observation data   总被引：4，自引：0，他引：4  

SHAN Xinjian  MA Jin  WANG Changlin  LIU Jiahang  SONG Xiaoyu & ZHANG Guifang .Institute of Geology  Laboratory of Tectonophysics  China Seismological Bureau  Beijing  China  .Institute of Remote Sensing Application  Chinese Academy of Sciences  Beijing  China 《中国科学D辑(英文版)》2004,47(6):481-488

In recent ten years, Differential Interferometric Synthetic Aperture Radar (D-InSAR) has become a major technique of space-based geodesy together with GPS, VLBI and SLR. Interferometric Synthetic Aper-ture Radar (InSAR) has many advantages, such as all-weather, all-time, strong stability and dynamic survey property, and no requirements for ground sta-tions. In particular, the surveying results by InSAR can cover a large range of the ground deformation field in succession and has gr…  相似文献   

Wind tunnel simulation experiment and investigation on the electrification of sandstorms     

QU Jianjun  YAN Muhong  DONG Guangrong  ZHANG Hongfa  ZU Ruiping  TUO Wanquan  ZHAO Aiguo  XlAO Zhenghua  LI Fang & YANG Bao Key Laboratory of Desert  Desertification  Cold  Arid Regions Environmental  Engineering Research Institute  Shapotou Desert Research  Experiment Station  Chinese Academy of Sciences  Lanzhou  China 《中国科学D辑(英文版)》2004,47(6):529-539

~~Wind tunnel simulation experiment and investigation on the electrification of sandstorms~~  相似文献   

Comparison of the dynamic response of a saturated soil between two models     

LIN Mian Institute of Mechanics  Chinese Academy of Sciences  Beijing  China 《中国科学D辑(英文版)》2004,47(6):551-558

The dynamic response of marine sediment to ocean surface waves is treated extremely by marine geotechnical and coastal engineers. In the area of conventional hydrodynamics, the assumption of im-permeable rigid seabed has been used as the boundary of water waves theories and the waves parameters de-duced from the theory have not referred to the interac-tion of water waves and seabed. In the area of soil mechanics, many engineers regard the response as slow loading according to the Zienkewiczs[1…  相似文献   

Palynological record during the Pleistocene (between 1.05 Ma and 0.36 Ma) from ODP1144, northern South China Sea     

HUANG Fei & SUN XiangjunInstitute of Geology  Paleontology  Chinese Academy of Sciences  Nanjing  China  Institute of Botany  Chinese Academy of Sciences  Beijing  China  Key Laboratory of Marine Geology  Ministry of Education  Tongji University  Shanghai  China Correspondence should be addressed to Huang Fei 《中国科学D辑(英文版)》2004,47(1):30-36

This paper presents the pollen record from the lower section of ODP1144 (depth 501.3-225.7 m, ca. 1.05-0.36 Ma). Two pollen zones (PA and PB) and eleven pollen subzones are recognized. Within zone PB, the 11 pollen subzones (PB21-11) are defined according to the pine, fern and herb variations, and are equivalent to the marine isotope stages 21-11 (MISs 21-11). The interglacial periods are typified by an increase in pine pollen and fern spores, and a decrease in herbaceous pollen, while the patterning during the glacial periods is just the opposite. During the interglacial periods, pollen assemblages were dominated by pine similar to those of the present day, suggesting that the paleoenvironment of the interglacial periods was similar to that of the present day, whereas the glacial periods are marked by an increase in herbaceous pollen, mainly Gramineae and Cyperaceae, indicating that grassland covered the exposed continental shelf when sea level declined. Increased Artemisia percentages and the highest  相似文献