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Was the enclosed Qaidam Basin of The Tibetan Plateau Accumulative or Erosive during the Late Quaternary?
Lai Zhongping1,2
2014-12-01
发表期刊ACTA GEOLOGICA SINICA-ENGLISH EDITION
卷号88页码:14-14
语种英语
引用统计
文献类型期刊论文
条目标识符http://ir.isl.ac.cn/handle/363002/5656
专题青海盐湖研究所知识仓储
盐湖地质与环境实验室
作者单位1.Chinese Acad Sci, Qinghai Inst Salt Lakes, Key Lab Salt Lake Resources & Chem, Xining 810008, Peoples R China
2.Chinese Acad Sci, Cold & Arid Reg Environm & Engn Res Inst, State Key Lab Cryosphere Sci, Lanzhou 730000, Peoples R China
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GB/T 7714
Lai Zhongping. Was the enclosed Qaidam Basin of The Tibetan Plateau Accumulative or Erosive during the Late Quaternary?[J]. ACTA GEOLOGICA SINICA-ENGLISH EDITION,2014,88:14-14.
APA Lai Zhongping.(2014).Was the enclosed Qaidam Basin of The Tibetan Plateau Accumulative or Erosive during the Late Quaternary?.ACTA GEOLOGICA SINICA-ENGLISH EDITION,88,14-14.
MLA Lai Zhongping."Was the enclosed Qaidam Basin of The Tibetan Plateau Accumulative or Erosive during the Late Quaternary?".ACTA GEOLOGICA SINICA-ENGLISH EDITION 88(2014):14-14.
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