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![]() |
刊名 | Tectonophysics
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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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