机译:LGM以来,青藏高原柴达木盆地风沙沉积受河流过程,气候变化和人类活动控制。
Linyi Univ, Coll Resources & Environm, Linyi 276000, Peoples R China|Qinghai Geol Survey Inst, Key Lab Geol Proc & Mineral Resources Northern Qi, Xining 810012, Peoples R China|Chinese Acad Sci, State Key Lab Cryospher Sci, Cold & Arid Reg Environm & Engn Res Inst, Lanzhou 730000, Peoples R China;
Chinese Acad Sci, State Key Lab Cryospher Sci, Cold & Arid Reg Environm & Engn Res Inst, Lanzhou 730000, Peoples R China|China Univ Geosci, Sch Earth Sci, Wuhan 430074, Peoples R China;
Qinghai Geol Survey Inst, Key Lab Geol Proc & Mineral Resources Northern Qi, Xining 810012, Peoples R China;
Qinghai Geol Survey Inst, Key Lab Geol Proc & Mineral Resources Northern Qi, Xining 810012, Peoples R China;
Chinese Acad Sci, Qinghai Inst Salt Lakes, Xining 810012, Peoples R China|Univ Chinese Acad Sci, Beijing 100049, Peoples R China;
OSL dating; Desert evolution; Palaeoenvironmental change; Human activity; Deglaciation and Holocene; Qinghai-Tibetan plateau;
机译:青藏高原东北部柴达木盆地湖相沉积物中Rb / Sr比值异常:风沙输入的重要作用
机译:青藏高原东北部柴达木盆地湖相沉积物的风成特征及其古气候意义
机译:青藏高原东北部柴达木盆地东部风沙沉积的OSL年代学和古气候意义
机译:青藏高原湖泊变化与全球气候变化关系的研究
机译:荧光纹理和水文演化和气候变化在年轻火山景观中的恢复力:Rhyolite Plateau和Lamar Valley,黄石国家公园
机译:揭露气候变化和人类活动对世界大河流向海岸的河流沉积物供应的相对影响:中国珠江流域
机译:密歇根州大河流域。综合水资源研究。第三卷。附录C.气候附录D.地表水水文和水力学和河流沉积物。