机译:千禧年夏季季风振荡在过去260 ka上,由曼山黄土高原莽山黄土 - 甘地源序列的高分辨率元素结果揭示
Chinese Acad Sci Inst Earth Environm State Key Lab Loess & Quaternary Geol Xian 710061 Peoples R China|Univ Chinese Acad Sci Beijing 100049 Peoples R China;
Chinese Acad Sci Inst Earth Environm State Key Lab Loess & Quaternary Geol Xian 710061 Peoples R China|Univ Chinese Acad Sci Beijing 100049 Peoples R China;
Northwest Univ Dept Geol State Key Lab Continental Dynam Shaanxi Key Lab Early Life & Environm Xian 710069 Peoples R China;
Chinese Acad Sci Guangzhou Inst Geochem Key Lab Ocean & Marginal Sea Geol Guangzhou 510640 Peoples R China;
Chinese Acad Sci Inst Earth Environm State Key Lab Loess & Quaternary Geol Xian 710061 Peoples R China;
Chinese Acad Sci Inst Earth Environm State Key Lab Loess & Quaternary Geol Xian 710061 Peoples R China|CAS Ctr Excellence Quaternary Sci & Global Change Xian 710061 Peoples R China;
Chinese loess; Elemental ratios; Millennial-scale; East Asian summer monsoon;
机译:河流漫滩的粉尘供应:以shan山高原黄土古土壤序列记录的黄河下游(黄河)为例
机译:中国河南黄河南部Man山黄土古土壤序列的新发光年表
机译:从Man山黄土古土壤序列和中国三门峡的湖相沉积物推断黄河的形成
机译:南海准两年一次涛动和夏季风对华南夏季降水年代际变化的影响
机译:末次冰期期间黄土高原西部高分辨率夏季降水变化
机译:河流漫滩的粉尘供应:以Man山高原黄土古土壤序列记录的黄河下游(黄河)为例