Channel flow of the lower crust and its relation to large-scale tectonic geomorphology of the eastern Tibetan Plateau

	Channel flow of the lower crust and its relation to large-scale tectonic geomorphology of the eastern Tibetan Plateau
	Wang XF (王晓芳) ; He JK (何建坤)
刊名	SCIENCE CHINA-EARTH SCIENCES
	2012
卷号	55 期号:8 页码:1383-1390
关键词	SLIP RATES DEFORMATION FAULT LITHOSPHERE COLLISION EXTENSION EXTRUSION STRENGTH SYSTEM KUNLUN
通讯作者	He, JK (通讯作者),Chinese Acad Sci, Key Lab Continental Collis & Plateau Uplift, Inst Tibetan Plateau Res, Beijing 100085, Peoples R China.
合作状况	其它
学科主题	地质学
收录类别	SCI
WOS记录号	WOS:000307255500019
公开日期	2013-05-23
内容类型	期刊论文
源URL	[http://ir.itpcas.ac.cn:8080/handle/131C11/2073]
专题	青藏高原研究所_图书馆
推荐引用方式 GB/T 7714	Wang XF ,He JK . Channel flow of the lower crust and its relation to large-scale tectonic geomorphology of the eastern Tibetan Plateau[J]. SCIENCE CHINA-EARTH SCIENCES,2012,55(8):1383-1390.
APA	Wang XF ,&He JK .(2012).Channel flow of the lower crust and its relation to large-scale tectonic geomorphology of the eastern Tibetan Plateau.SCIENCE CHINA-EARTH SCIENCES,55(8),1383-1390.
MLA	Wang XF ,et al."Channel flow of the lower crust and its relation to large-scale tectonic geomorphology of the eastern Tibetan Plateau".SCIENCE CHINA-EARTH SCIENCES 55.8(2012):1383-1390.