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east antarctica     
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  东南极
     The 4000year variation of sulfur,index for biological activity,in sediments of Xihu Lake,west Antarctica and Lake Nella,east Antarctica is compared with that of CH3SO-3,index for marine biological activity,in D10 ice core.
     以硫元素浓度作为湖相沉积物中生物活动强度的指标,对比了西南极长城站地区西湖沉积物和东南极中山站奈拉湖沉积物中生物活动强度的变化趋势,并与D10冰芯中反映海洋生物活动强度的指标CH3SO-3的浓度变化趋势作对比。
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     Calculations of the Balance-flux Distributions of the Lambert Glacier-Amery Ice Shelf System, East Antarctica
     东南极Lambert冰川—Amery冰架系统平衡通量分布的计算
短句来源
     Preliminary Results of the Inland Expeditions along a Transect from the Zhongshan Station to Dome A, East Antarctica
     东南极冰盖中山站——Dome A断面路线考察的初步结果
短句来源
     Snow Density and Stratigraphy at LGB65 in Princess Elizabeth Land, East Antarctica
     东南极伊利莎白公主地LGB65点的雪层密度与剖面特征
短句来源
     Boron isotopic compositions of borosilicates from the Larsemann Hills, East Antarctica
     东南极拉斯曼丘陵富硼岩系中硅硼镁铝矿-柱晶石-电气石矿物的硼同位素组成及其意义
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  东南极冰盖
     Preliminary Results of the Inland Expeditions along a Transect from the Zhongshan Station to Dome A, East Antarctica
     东南极冰盖中山站——Dome A断面路线考察的初步结果
短句来源
     A Primary Study on Ionic Concentrations in Snow Pitsin the Hinterland of East Antarctica
     东南极冰盖内陆深处几个雪坑离子浓度的初步研究
短句来源
     Snow density measurement and stratigraphic observation of a 50 m firn-core and a snow-pit at LGB65 in Princess Elizabeth Land, East Antarctica, were conducted. The major conclusions were obtained as follows: (1) Densification of snow/firn belongs to cold type one. The depths of the first and the second critical density are 10.4 m and 60.4 m respectively.
     对东南极冰盖伊利莎白公主地LGB6 5点的 5 0m雪芯及雪坑进行了雪层密度与剖面分析 ,结果表明 ,该处雪的密实化过程属冷型密实化类型 ,第一和第二临界密度深度分别为 10 4m和 6 0 4m .
短句来源
  东南极内陆
     POST DEPOSITIONAL MODIFICATION OF NO - 3 IN SNOW LAYERS AT EAST ANTARCTICA AND AT THE HEADWATER OF URUMCHI RIVER
     东南极内陆地区和乌鲁木齐河源1号冰川表层雪内NO_3~-沉积后过程差异
短句来源
     Exposure ages of bedrock samples taken from two nunataks in the Grove Mountains (GMs), interior East Antarctica, are studied by dating in situ produced cosmogenic 10Be and 26Al. The results indicate that the minimum exposure time of the five samples are all about 2Ma, much older than that of Last Glacial Maximum.
     采自东南极内陆格罗夫山地区两个冰原岛峰的五个基岩样品的原地生成宇宙成因核素1 0 Be和2 6Al测试结果表明 ,这五个样品的最小暴露年龄都在 2Ma左右 ,远远早于末次冰期极盛期 (LGM )。
短句来源
     Mafic granulites and amphibolites crop out in the Grove Mountains (GMs), 450km s outh of Zhongshan Station on the coast of Prydz Bay, East Antarctica.
     东南极内陆 -格罗夫山存在一套经历了麻粒岩相变质作用的镁铁质麻粒岩和斜长角闪岩。
短句来源
     BEDROCK EXPOSURE AGES IN THE GROVE MOUNTAINS, INTERIOR EAST ANTARCTICA
     东南极内陆格罗夫山地区基岩暴露年龄研究
短句来源
     Presently, most research is concentrated on the coastal ice shelves of WAIS (West Antarctic Ice Sheet), very few work has been done for in-land glaciers in East Antarctica.
     目前的研究重点主要在西南极沿岸冰架地区,东南极内陆冰盖地区涉足很少。
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  南极内陆
     BEDROCK EXPOSURE AGES IN THE GROVE MOUNTAINS, INTERIOR EAST ANTARCTICA
     东南极内陆格罗夫山地区基岩暴露年龄研究
短句来源
     EVIDENCE FOR EAST ANTARCTIC ICE SHEET DEVELO-PMENT AND PALAEOCLIMATIC EVOLUTION FROM THE GROVE MOUNTAINS,EAST ANTARCTICA
     东南极内陆格罗夫山地区新生代冰川活动和古气候演化记录
短句来源
     Presently, most research is concentrated on the coastal ice shelves of WAIS (West Antarctic Ice Sheet), very few work has been done for in-land glaciers in East Antarctica.
     目前的研究重点主要在西南极沿岸冰架地区,东南极内陆冰盖地区涉足很少。
短句来源
     Mafic granulites and amphibolites crop out in the Grove Mountains (GMs), 450km s outh of Zhongshan Station on the coast of Prydz Bay, East Antarctica.
     东南极内陆 -格罗夫山存在一套经历了麻粒岩相变质作用的镁铁质麻粒岩和斜长角闪岩。
短句来源
     Exposure ages of bedrock samples taken from two nunataks in the Grove Mountains (GMs), interior East Antarctica, are studied by dating in situ produced cosmogenic 10Be and 26Al. The results indicate that the minimum exposure time of the five samples are all about 2Ma, much older than that of Last Glacial Maximum.
     采自东南极内陆格罗夫山地区两个冰原岛峰的五个基岩样品的原地生成宇宙成因核素1 0 Be和2 6Al测试结果表明 ,这五个样品的最小暴露年龄都在 2Ma左右 ,远远早于末次冰期极盛期 (LGM )。
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      east antarctica
    Magmatism of the Karoo-Maud superplume in the Schirmacher Oasis, East Antarctica
          
    Charnockites from East Antarctica and their geological typification
          
    Discovery of sapphirine-bearing hyperthene quartzite in the Larsemann Hills, East Antarctica, and its geological significance
          
    Nd, Sr, and Pb Isotope systematics of ultramafic rocks from the lasermann hills, East Antarctica
          
    Neoproterozoic magmatism in Southern India, Madagascar and East Antarctica : Implications to the breakup of Rodinia
          
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    This paper describes the results of observation on the fluxes of momentum and sensible heat over Mizuho Station (70°41' 53 " S, 44°19 ' 54 " E), East Antarctica. The data were collected by using the meteorological tower 32m high at this station in 1979-1981 period. These fluxes were evaluated by semiemperical flux-profile relation of Monin-Obukhov similarity theory from these observed data, and the calculated result was compared with that over the West Pacific Tropical Ocean area and Beijing area.

    本文根据南极瑞穗站气温、风等平均廓线资料,利用相似理论通量一廓线关系计算得出了该站的湍流通量,并与西太平洋热带海域和北京地区湍流通量计算结果进行了比较。

    The detailed studies of firn grain mean area at 16 sites on Law Dome, East Antarctica, indicate that the enhanced grain growth in the several metres neai the snow surface is more apparent in low accumulation areas, declining with the increase of accumulation rate. This can be contributed to the short staying period of the snow near the surface caused by the higher accumulation rate. The variation of mean grain area with both depth and age can be approximately represented by linear relations. The rate of...

    The detailed studies of firn grain mean area at 16 sites on Law Dome, East Antarctica, indicate that the enhanced grain growth in the several metres neai the snow surface is more apparent in low accumulation areas, declining with the increase of accumulation rate. This can be contributed to the short staying period of the snow near the surface caused by the higher accumulation rate. The variation of mean grain area with both depth and age can be approximately represented by linear relations. The rate of increase of mean area versus depth decreases markedly with accumulation rates due to the very large differences in accumulation rates between the sampling sites. Growth rate versus temperature at about-17癈 starts to depart from the temperature dependence of crystal growth rate established by Gow (1975) suggesting that the activation energy for the growth process increases with increasing temperature.

    对东南极洛多姆冰帽16个地点粒雪晶粒平均面积的详细研究表明,表层数米内晶粒的迅速生长在低积累区较为显著,随积累率增大逐渐减弱,原因可能是随积累率增大粒雪在近表层停留时间变短。晶粒平均面积随深度及年代的变化都可以较好地用线性关系近似表示。由于采样地点间积累率的巨大差别,积累率对晶粒平均面积深度关系影响较大。随积累率增加,晶粒平均面积的增加速率随深度明显减小。晶粒生长速率随温度的关系在-17℃左右开始和Gow(1975)的关系偏离,反映出晶粒生长过程的自扩散激活能可能和温度有关,其值随温度升高而增大。

    Ice crystals were measured from a marginal ice core from East Antarctica. The climatic significance related to ice crystals was discussed. A comparison was made between the Dunde ice core results and other ice core results. Based on the changes of ice crystals along the depth and the ubrupt changes of ice crystals during the Last Ice Age, it was concluded that climate can not only affect the growth rate of ice crystals, but also affect ice crystal size under specific climatic condition (e. g. Last Ice...

    Ice crystals were measured from a marginal ice core from East Antarctica. The climatic significance related to ice crystals was discussed. A comparison was made between the Dunde ice core results and other ice core results. Based on the changes of ice crystals along the depth and the ubrupt changes of ice crystals during the Last Ice Age, it was concluded that climate can not only affect the growth rate of ice crystals, but also affect ice crystal size under specific climatic condition (e. g. Last Ice Age). The fact that climatic information can be reserved in marginal ice of ice sheet indicates that the conclusion that ice crystal growth rate can be