机译:δ〜(18)O记录与石笋中痕量元素比率之间的不一致:干旱中亚全新世中晚期全新世水分增加的证据
Chinese Acad Sci Inst Tibetan Plateau Res Key Lab Alpine Ecol & Biodivers LAEB 16 Lincui Rd Beijing 100101 Peoples R China;
Chinese Acad Sci Inst Tibetan Plateau Res Key Lab Alpine Ecol & Biodivers LAEB 16 Lincui Rd Beijing 100101 Peoples R China|Lanzhou Univ Coll Earth & Environm Sci Minist Educ Key Lab West Chinas Environm Syst Lanzhou Gansu Peoples R China|Chinese Acad Sci CAS Ctr Excellence Tibetan Plateau Earth Syst Sci Beijing Peoples R China;
Natl Taiwan Univ Dept Geosci High Precis Mass Spectrometry & Environm Change L Taipei Taiwan|Natl Taiwan Univ Res Ctr Future Earth Taipei Taiwan;
Southwest Univ Sch Geog Sci Chongqing Key Lab Karst Environm Chongqing Peoples R China;
Lanzhou Univ Coll Earth & Environm Sci Minist Educ Key Lab West Chinas Environm Syst Lanzhou Gansu Peoples R China;
Nanyang Technol Univ Earth Observ Singapore Singapore Singapore|Nanyang Technol Univ Asian Sch Environm Singapore Singapore;
arid central Asia; Holocene moisture; precipitation; inconsistent trends; speleothem delta O-18; speleothem trace element ratios; westerlies circulation;
机译:中国北部全新世东亚夏季风记录及其与中国石笋三角洲O-18记录的不一致
机译:从华中神农架的石笋δ〜(18)O记录推断全新世亚洲季风的长期趋势和突变事件
机译:中亚中亚全新世夏季降水的趋势:来自新疆LJW10黄土段有机碳同位素记录的证据,NW中国
机译:从拉古斯汀碳酸盐的氧同位素记录推断,全新世期间瑞典北部整个斯坎德山脉的水分输送效率变化的证据
机译:白垩纪年龄的亨塞尔古土壤的氧同位素,微量元素和沉积学表明德克萨斯州中部的干旱和气温上升
机译:博茨瓦纳中部近地表半干旱土壤微量元素PXRF数据集的地统计学分析
机译:中亚中亚中亚的全新世水分变化,从石笋推断出来