机译:过去550,000年的中纬度半球水文跷跷板
Korea Institute of Geoscience and Mineral Resources, Daejeon 305-350, South Korea;
Department of Geology, Kangwon National University, Gangwondo 200-701, South Korea;
Korea Institute of Geoscience and Mineral Resources, Daejeon 305-350, South Korea;
Korea Institute of Geoscience and Mineral Resources, Daejeon 305-350, South Korea;
Department of Geological Sciences, Pusan National University, Busan 609-735, South Korea;
College of Geography Science, Nanjing Normal University, Nanjing 210097, China;
Institute of Global Environmental Change, Xi'an Jiaotong University, Xi'an 710049, China,Department of Geology and Geophysics, University of Minnesota, Minneapolis, Minnesota 55455, USA;
Department of Geology and Geophysics, University of Minnesota, Minneapolis, Minnesota 55455, USA;
机译:双极跷跷板是否延伸到陆地南部中纬度?
机译:中纬度地区最后一个冰川最大值的近同步半球间终止
机译:一种南海海洋机制,用于互动的互动耦合和双极跷跷板的阶段
机译:水文工程中心-水文工程史五十年
机译:过去20,000年的热带大西洋SST:对半球间气候变化的机制和同步性的影响。
机译:最近两千年的热带降雨:低纬水文跷跷板的证据
机译:中纬离子密度的经纬变化中的互脱串联效应
机译:近500年来佛得角盆地深海底栖动物有孔虫和海水碳酸盐饱和度及底栖有孔虫碳酸盐饱和度历史