搜索结果: 1-15 共查到“地球物理学 Mw=8.3”相关记录17条 . 查询时间(0.062 秒)
ESTIMATION OF CO- AND POSTSEISMIC DEFORMATION AFTER THE Mw 8.6 NIAS-SEMEULUE AND Mw 8.5 BENGKULU EARTHQUAKES FROM CONTINUOUS GPS DATA
GPS earthquake postseismic deformation
2016/10/14
The Mw 8.5 Bengkulu earthquake of 30 September 2007 and the Mw8.6 28 March 2005 are considered amongst large earthquake ever recorded in Southeast Asia. The impact into tectonic deformation was record...
The April 6, 2009, Mw 6.3, L'Aquila sequence: weak-motion and strong-motion data recorded by the RAIS temporary stations
Surveys measurements and monitoring Seismological data L'Aquila earthquake Aftershocks
2015/8/28
The aim of this study is the sharing of waveforms recorded by several Istituto Nazionale di Geofisica e Vulcanologia (INGV) temporary stations (managed by the Milan-Pavia section; INGV MI-PV). These s...
Source complexity of the May 20,2012,Mw 5.9,Ferrara (Italy) event
Empirical Green's functions Array analysis
2015/8/26
A Mw 3.9 foreshock on May 19, 2012, at 23:13 UTC, was followed at 02:03 on May 20, 2012, by a Mw 5.9 earthquake that hit a densely populated area in the Po Plain, west of the city of Ferrara, Italy (F...
A teleseismic finite-fault rupture model for the August 17,1999,304;zmit earthquake (Mw = 7.6): implications for the seismic nucleation phase
North Anatolian Fault 1999 İ zmit earthquake Rupture process Slip distribution Rupture nucleation
2015/8/24
A linear finite-fault inversion procedure is applied to teleseismically recorded broadband P and SH velocity waveforms of the August 17, 1999, İzmit earthquake, to derive spatial and temporal dis...
Wave-equation-based travel-time seismic tomography – Part 2: Application to the 1992 Landers earthquake (Mw 7.3) area
High resolution 3 d P wave S wave crust velocity poisson's ratio model landers earthquake earthquake fault
2015/1/6
High-resolution 3-D P and S wave crustal velocity and Poisson's ratio models of the 1992 Landers earthquake (Mw 7.3) area are determined iteratively by a wave-equation-based travel-time seismic tomogr...
On the complexity of surface ruptures during normal faulting earthquakes: excerpts from the 6 April 2009 L'Aquila (central Italy) earthquake (Mw 6.3)
On the complexity surface ruptures normal faulting earthquakes L'Aquila earthquake
2015/1/6
Over the past few years the assessment of the earthquake potential of large continental faults has increasingly relied on field investigations. State-of-the-art seismic hazard models are progressively...
DInSAR Coseismic Deformation of the May 2011 Mw 5.1 Lorca Earthquake (southeastern Spain)
DInSAR Coseismic Deformation Earthquake
2015/1/4
The coseismic superficial deformation at the region of Lorca (Murcia, southeastern Spain) due to the Mw
5.1 earthquake on 11 May 2011 was characterized by a multidisciplinary team, integrating ...
DInSAR Coseismic Deformation of the May 2011 Mw 5.1 Lorca Earthquake (southeastern Spain)
DInSAR Coseismic Deformation the May 2011 Mw 5.1 Lorca Earthquake
2015/1/4
The coseismic superficial deformation at the region of Lorca (Murcia, southeastern Spain) due to the Mw 5.1 earthquake on 11 May 2011 was characterized by a multidisciplinary team, integrating informa...
基于法国DEMETER卫星ISL探测器升轨数据，统计分析了2005—2009年全球37个Mw≥7.0级地震前后电离层电子浓度变化.结果发现，共有19个地震（51%）前观测到了较为明显的电子浓度异常扰动现象，其中大部分表现为异常增强；观测到的电子浓度异常现象一般出现在震前1~5天内，也有部分地震前出现两次及以上扰动现象.分析表明，在赤道和中低纬地区更容易观测到明显的电子浓度扰动，即异常震例基本发生在...
Low friction along the high slip patch of the 2011 Mw 9.0 Tohoku-Oki earthquake required from the wedge structure and extensional splay faults
Low friction along the high slip patch 2011 Mw 9.0 Tohoku-Oki earthquake required the wedge structure extensional splay faults
2014/4/15
We analyze the mechanical properties needed to account for the large shallow slip during the 2011 Tohoku-Oki earthquake and the activation of landward normal faulting within the forearc. We show that ...
中国科学院测量与地球物理研究所利用GPS位移反演日本Mw 9.0仙台地震及Mw7.9强余震静态位错模型（图）
中国科学院测量与地球物理研究所 GPS位移 日本Mw 9.0仙台地震 Mw7.9强余震 静态位错模型
2011/10/26
Mw 9.0 日本仙台地震发生后，中科院测地所地震与地球动力学学科组刁法启博士生在导师熊熊研究员指导下，利用GPS观测的Mw 9.0日本仙台地震同震形变及震后8小时的地表形变[1],考虑分层介质模型的影响, 快速反演了主震及震后8小时的断层的位错分布. 结果显示, 主震的位错模型对应的矩震级为Mw 8.98, 最大同震位错量可达24 m, 在震中区显示出纯逆冲特性, 震中两侧断层错动显示出一定的走...
据覆盖日本全境的GEONET 网络GPS 观测资料显示, 2011 年3 月11 日的日本宫城MW9.0 级地震造成日本半岛向东移动, 最大达到了5.3 m. 利用国家重大科技基础设施项目“中国大陆构造环境监测网络”的GPS 观测资料, 分析此次地震对中国大陆构造形变场的同震影响,结果显示, 地震造成我国东北和华北地区产生毫米至厘米级的同震水平位移, 最大值为35 mm.通过应变分析发现, 地震导...
2011年3月11日日本宫城Mw 9.0 级大震后的两天九州岛上新燃岳火山发生大规模喷发. 此次火山喷发是否是受地震触发所致, 以及地震是否同样也会造成富士山火山和长白山火山的喷发成为人们关注的热点. 通过对地震造成的区域应力应变场的计算, 发现富士山火山、新燃岳火山和长白山火山均处于体膨胀区, 在地下10 km 处体膨胀分别达到~220, ~8 和~14 nano-strain. 由同震GPS ...
Brief communication "Report on the impact of the 27 February 2010 earthquake (Chile, Mw 8.8) on rockfalls in the Las Cuevas valley, Argentina"
Brief communication earthquake rockfalls Las Cuevas valley
2010/10/21
Numerous rockfalls were detected in the Las Cuevas valley, Argentina, after the 27 February 2010 earthquake in Chile. Live rockfalls were observed during aftershocks of 11 March 2010. Many rockfall so...
Kinematics of the November 12, 1999 (Mw=7.2) Düzce Earthquake Deduced from SAR Interferometry
Düzce earthquake SAR Interferometry GPS elastic modelling source parameters
2009/7/8
On November 12 1999, a destructive earthquake struck the Düzce area, following the 17 August 1999 İzmit earthquake that had occurred to the west about 3 months earlier. The Mw=7.2 Düzce earthqua...