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	Gradual late stage deepening of Gega ice-dammed lake, Tsangpo gorge, southeastern Tibet, indicated by preliminary sedimentary rock magnetic properties
	Liu, Weiming; Zhou, Gordon G. D.; Ge, Yonggang; Huang, Runqiu
	2018
卷号	66期号:5页码:907-914
URL标识	查看原文
WOS记录号	WOS:000448505400006
内容类型	期刊论文
URI标识	http://www.corc.org.cn/handle/1471x/4378261
专题	成都理工大学
作者单位	1.[1]Chinese Acad Sci, Inst Mt Hazards & Environm, CAS Key Lab Mt Hazards & Surface Proc, Chengdu 610041, Sichuan, Peoples R China 2.[2]Chengdu Univ Technol, State Key Lab Geohazard Prevent & Geoenvironm Pro, Chengdu 610041, Sichuan, Peoples R China
推荐引用方式 GB/T 7714	Liu, Weiming,Zhou, Gordon G. D.,Ge, Yonggang,et al. Gradual late stage deepening of Gega ice-dammed lake, Tsangpo gorge, southeastern Tibet, indicated by preliminary sedimentary rock magnetic properties[J],2018,66(5):907-914.
APA	Liu, Weiming,Zhou, Gordon G. D.,Ge, Yonggang,&Huang, Runqiu.(2018).Gradual late stage deepening of Gega ice-dammed lake, Tsangpo gorge, southeastern Tibet, indicated by preliminary sedimentary rock magnetic properties.,66(5),907-914.
MLA	Liu, Weiming,et al."Gradual late stage deepening of Gega ice-dammed lake, Tsangpo gorge, southeastern Tibet, indicated by preliminary sedimentary rock magnetic properties".66.5(2018):907-914.

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