Was the enclosed Qaidam Basin of The Tibetan Plateau Accumulative or Erosive during the Late Quaternary?

ISL OpenIR > 青海盐湖研究所知识仓储

	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
推荐引用方式 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.