Results 171 to 180 of about 5,289,635 (205)
International Journal of Earth Sciences, 2017 Intraplate earthquakes pose a significant seismic hazard in densely populated rift systems like the Lower Rhine Graben in Central Europe. While the locations of most faults in this region are well known, constraints on their seismogenic potential and earthquake recurrence are limited.
Simon Kübler +3 more
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Acta Geologica Sinica, 2012
Abstract:On 21 March 2008, a Ms7.3 earthquake occurred at Quickbird, Yutian County, Xinjiang. We attempt to reveal the features of the causative fault of this shock and its coseismic deformation field. Our work is based on analysis and interpretation to high‐resolution satellite images as well as differential interferometric synthetic aperture radar (D‐
Qu Chunyan, Xinjian Shan, Chisheng Wang
exaly +2 more sources
Abstract:On 21 March 2008, a Ms7.3 earthquake occurred at Quickbird, Yutian County, Xinjiang. We attempt to reveal the features of the causative fault of this shock and its coseismic deformation field. Our work is based on analysis and interpretation to high‐resolution satellite images as well as differential interferometric synthetic aperture radar (D‐
Qu Chunyan, Xinjian Shan, Chisheng Wang
exaly +2 more sources
Tectonophysics, 2010
Abstract The May 12, 2008, Mw 7.9 Wenchuan earthquake occurred along the Longmen Shan fault zone, a thrust fault zone on the eastern margin of Tibet Plateau, and ruptured the ground surface for more than 200 km. A field investigation suggests that the earthquake also ruptured the northern segment (from Beichuan to Qingchuan), along which active ...
Chuan-You Li +4 more
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Abstract The May 12, 2008, Mw 7.9 Wenchuan earthquake occurred along the Longmen Shan fault zone, a thrust fault zone on the eastern margin of Tibet Plateau, and ruptured the ground surface for more than 200 km. A field investigation suggests that the earthquake also ruptured the northern segment (from Beichuan to Qingchuan), along which active ...
Chuan-You Li +4 more
exaly +2 more sources
In chapter 2 we describe a novel estimation methodology for estimating coseismic slip models from geodetic observations of coseismic surface deformation. We apply our method to observations from the August 9, 2020, M$_{w}$ 5.1 Sparta, North Carolina earthquake captured by ALOS-2 and Sentinel 1A/B interferograms, along with differential LiDAR.
Szymanski, Eric
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Journal of Geophysical Research F: Earth Surface, 2019 The 2016 central Apennines earthquake sequence was caused by slip on an extensional faultsystem and resulted in sizable coseismic surface deformation.
Carlo Esposito +2 more
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Coseismic surface deformation caused by the Wenchuan M8 earthquake from InSAR data analysis
2009 IEEE International Geoscience and Remote Sensing Symposium, 2009The D-InSAR technology is used to aquired seven belts of coseismic surface deformation of Sichuan M8 earthquake of 12 May 2008 from the ALOS/PALSAR satellite data of Japan. The result covers Yinxiu, Dujiangyan, Wenchuan, Moxian, Beichuan, Pingwu and Qingchuan county, each 500km in north-south and 70km in east-west.
Xiaogang Song 0002 +5 more
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Direct estimation of rupture depths of earthquake faults from coseismic surface deformation
Science China Earth Sciences, 2014The rupture dimensions of earthquake faults are important parameters for characterizing earthquake ruptures and ground motions. Two key parameters to be determined are the rupture depth and dip angle of earthquake faults. Dislocation theory in an elastic half space indicates that if a seismic rupture directly runs up to the ground surface, there exist ...
Zhen Fu +4 more
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Remote Sensing, 2023 The largest earthquake (Mw 6.4) in northwestern Croatia ruptured the faults near the city of Petrinja on 29 December 2020, at 11:19 UTC. The epicenter was located ~3 km southwest of Petrinja, ~40 km southeast of Zagreb, the capital of the Republic of ...
Jingbin Liu, Yangmao Wen, Sen Zhu
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Proceedings 2011 IEEE International Conference on Spatial Data Mining and Geographical Knowledge Services, 2011
On 9 January, 2008, the Mw 6.4 earthquake occurred in Gaize, central Tibet of China, then the largest aftershock Mw 5.9 followed on 16th of January. Firstly, we derive the co-seismic deformation field with Synthetic Aperture Radar. The results show an asymmetric deformation pattern both mainshock and aftershock with normal faulting on a NE-striking ...
Guifang Zhang +3 more
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On 9 January, 2008, the Mw 6.4 earthquake occurred in Gaize, central Tibet of China, then the largest aftershock Mw 5.9 followed on 16th of January. Firstly, we derive the co-seismic deformation field with Synthetic Aperture Radar. The results show an asymmetric deformation pattern both mainshock and aftershock with normal faulting on a NE-striking ...
Guifang Zhang +3 more
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Izvestiya, Atmospheric and Oceanic Physics, 2018
The occurrence time prediction of the strongest earthquakes is one of most topical tasks of seismology. Appearing in the recent years, new observation methods for precursors of different nature can open avenues to achieve success in the field of medium-term seismic forecast. One such method is to observe the Earth’s surface deformation using the Global
null Jiao Liu, E. A. Rogozhin
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The occurrence time prediction of the strongest earthquakes is one of most topical tasks of seismology. Appearing in the recent years, new observation methods for precursors of different nature can open avenues to achieve success in the field of medium-term seismic forecast. One such method is to observe the Earth’s surface deformation using the Global
null Jiao Liu, E. A. Rogozhin
openaire +1 more source