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机译:圆顶C和圆顶富士冰岩的组成,从上次冰川最大到全新世,基于冰升华和单粒子测量
National Institute of Polar Research Research Organization of Information and Systems Tokyo Japan;
Institute of Low Temperature Science Hokkaido University Sapporo Japan;
National Institute of Polar Research Research Organization of Information and Systems Tokyo Japan;
Department of Earth Sciences University of Cambridge Cambridge UK;
Department of Chemistry "Ugo Schiff" University of Florence Florence Italy;
Japan Agency for Marine-Earth Science and Technology Yokohama Japan;
National Institute of Polar Research Research Organization of Information and Systems Tokyo Japan;
Department of Physical Geography Stockholm University Stockholm Sweden;
Compositions; Dust and Sea; Salts;
机译:圆顶C和圆顶富士冰岩的组成,从上次冰川最大到全新世,基于冰升华和单粒子测量
机译:富士圆顶(南极洲)冰芯表现出的最后一次冰期最大值期间的不溶和不挥发颗粒的组成元素
机译:Na2SO4和MgSO4盐在全茂期间通过高分辨率深度分析来源的圆顶富士冰芯
机译:东南极地区的圆顶富士站和日本南极研究探险
机译:Siple Dome冰芯的稳定同位素和氘过量:对南极罗斯海地区第四纪晚期气候和海拔历史的影响。
机译:形状和尺寸限制了南极Dome C冰芯的尘埃光学特性
机译:圆顶C和圆顶富士冰岩的组成,从上次冰川最大到全新世,基于冰升华和单粒子测量