中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
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

文献类型:期刊论文

作者Wang Q; Ji SC; Salisbury MH; Xia B; Pan MB; Xu ZQ
刊名Tectonophysics
出版日期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
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.

入库方式: OAI收割

来源:广州地球化学研究所

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