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您的检索式：作者名="Sanming Luo"
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| 1 | Co- and post-seismic vertical displacements of Wenchuan Ms8.0 earthquake near Beichuan显示文摘Co-and post-seismic vertical displacements of the Wenchuan earthquake derived from two measurements in 2008 and 2010 along two partly-damaged leveling lines near the epicenter show the following features:Co-seismic displacement at Beichuan-Yingxiu fault was as large as 4.711 m near Beichuan,where the maximum observed fault offset was 5.1 m.In contrast,the observed co-seismic offset of the Qingchuan fault in Pingwu County was only 0.064 m.During 2008-2010,the post-seismic displacement rate was 5-27 mm/a near Beichuan-Yingxiu fault in Beichuan area,20.6 mm/a at Jiangyou-Guangyuan fault near Dakang,and only 0.2-1.3 mm/a at Qingchuan fault near Gucheng. | Dong Yunhong Luo Sanming Han Yueping Chen Changyun | 2011 | Geodesy and Geodynamics2011，2，2： | 2 |
| 2 | Processes of the displacement field change of the 2009 April 6 M_W6.3 L'Aquila earthquake using persistent scatterer and small baseline methods显示文摘Using a time series method that combines both the persistent scatterer and small baseline approaches,we analyzed 9 scenes Envisat ASAR data over the L’Aquila earthquake,and obtained a Shocke’s displacement field and its evolution processes.The results show that:(1)Envisat ASAR clearly detected the whole processes of displacement field of the L’Aquila earthquake,and distinct variations at different stages of the displacement field.(2)Preseismic creep displacement?displacement mutation when faulting?constantly slowed down after the earthquake.(3)The area of the strongest deformation and ground rupture was a low-lying oval depression region to the southeast.Surface faulting within a zone of about22 km 9 14 km,with an orientation of 135°,occurred along the NW-striking and SW-dipping Paganica-S.Demetrio normal fault.(4)In analyzing an area of about54 km 9 59 km,bounded by north–south axis to the epicenter,the displacement field has significant characteristics of a watershed:westward of the epicenter shows uplift with maximum of 130 mm in line-of-sight(LOS),and east of the epicenter was a region with 220 mm of maximum subsidence in the LOS,concentrating on the rupture zone,the majority of which formed in the course of faulting and subsequence. | Sanming Luo Liming Fu Shuang Zhu Qinglong He Wenni Wan Bo Yang | 2013 | Earthquake Science2013，26，5： | 0 |
| 3 | Global plate motion and earthquake activity显示文摘全球板运动率不是在时空的制服。旋转率比 0.545 大 ?畦 n ???? | Yanxing Li Xiwu Luan Yuanzhong Lu Jinghua Zhang Hong Liu Sanming Luo Feng Liu | 2010 | Geodesy and Geodynamics2010，1，1： | 0 |
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