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	Marine Isotope Stage 3 paleotemperature inferred from reconstructing the Die Shan ice cap, northeastern Tibetan Plateau
	Cui, Hang[1,2]; Wang, Jie[1]; Yu, Beibei[1]; Hu, Zhenbo[1]; Yao, Pan[1]; Harbor, Jonathan M.[3]
	2018
卷号	89期号:2页码:494
URL标识	查看原文
WOS记录号	WOS:000430317400009
内容类型	期刊论文
URI标识	http://www.corc.org.cn/handle/1471x/5848182
专题	青海师范大学
作者单位	1.[1]Lanzhou Univ, Coll Earth & Environm Sci, Minist Educ, Key Lab Western Chinas Environm Syst, Lanzhou 730000, Gansu, Peoples R China 2.[2]Qinghai Normal Univ, Key Lab Phys Geog & Environm Proc Qinghai Prov, Xining 810008, Qinghai, Peoples R China 3.[3]Purdue Univ, Dept Earth Atmospher & Planetary Sci, W Lafayette, IN 47907 USA
推荐引用方式 GB/T 7714	Cui, Hang[1,2],Wang, Jie[1],Yu, Beibei[1],et al. Marine Isotope Stage 3 paleotemperature inferred from reconstructing the Die Shan ice cap, northeastern Tibetan Plateau[J],2018,89(2):494.
APA	Cui, Hang[1,2],Wang, Jie[1],Yu, Beibei[1],Hu, Zhenbo[1],Yao, Pan[1],&Harbor, Jonathan M.[3].(2018).Marine Isotope Stage 3 paleotemperature inferred from reconstructing the Die Shan ice cap, northeastern Tibetan Plateau.,89(2),494.
MLA	Cui, Hang[1,2],et al."Marine Isotope Stage 3 paleotemperature inferred from reconstructing the Die Shan ice cap, northeastern Tibetan Plateau".89.2(2018):494.

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