Pressure dependence and anisotropy of P-wave velocities in ultrahigh-pressure metamorphic rocks from the Dabie-Sulu orogenic belt (China): Implications for seismic properties of subducted slabs and origin of mantle reflections

CORC > 广州地球化学研究所 > 中国科学院广州地球化学研究所 > 中科院广州地化所(-2008)

	Pressure dependence and anisotropy of P-wave velocities in ultrahigh-pressure metamorphic rocks from the Dabie-Sulu orogenic belt (China): Implications for seismic properties of subducted slabs and origin of mantle reflections
	Wang Q; Ji SC; Salisbury MH; Xia B; Pan MB; Xu ZQ
刊名	Tectonophysics
	2005
卷号	398 期号:1-2 页码:67-99
ISSN号	0040-1951
语种	英语
WOS记录号	WOS:000228194100004
公开日期	2011-08-18
内容类型	期刊论文
源URL	[http://210.77.94.230:8080/handle/344008/12754]
专题	广州地球化学研究所_中科院广州地化所(-2008)
推荐引用方式 GB/T 7714	Wang Q,Ji SC,Salisbury MH,et al. Pressure dependence and anisotropy of P-wave velocities in ultrahigh-pressure metamorphic rocks from the Dabie-Sulu orogenic belt (China): Implications for seismic properties of subducted slabs and origin of mantle reflections[J]. Tectonophysics,2005,398(1-2):67-99.
APA	Wang Q,Ji SC,Salisbury MH,Xia B,Pan MB,&Xu ZQ.(2005).Pressure dependence and anisotropy of P-wave velocities in ultrahigh-pressure metamorphic rocks from the Dabie-Sulu orogenic belt (China): Implications for seismic properties of subducted slabs and origin of mantle reflections.Tectonophysics,398(1-2),67-99.
MLA	Wang Q,et al."Pressure dependence and anisotropy of P-wave velocities in ultrahigh-pressure metamorphic rocks from the Dabie-Sulu orogenic belt (China): Implications for seismic properties of subducted slabs and origin of mantle reflections".Tectonophysics 398.1-2(2005):67-99.