The results of Global Navigational Satellite System (GNSS) observations in the regions of large earthquakes are analyzed. The characteristics of the Earth’s surface deformations before, during, and after the earthquakes are considered. The obtained results demonstrate the presence of anomalous deformations close to the epicenters of the events. Statistical estimates of the anomalous strains and their relationship with measurement errors are obtained. Conclusions are drawn about the probable use of local GNSS networks to assess the risk of the occurrence of strong seismic events. © 2018, Pleiades Publishing, Ltd
Studies of GPS data carried out before and after the great Wenchuan earthquake of Ms8.0 on May 12, 2...
We have developed a global earthquake monitoring system based on low‐latency measurements from more ...
Monitoring earthquakes to rapidly forecast their consequences remains a challenging task, especially...
The results of Global Navigational Satellite System (GNSS) observations in the regions of large eart...
The results of observation of Global Navigation Satellite Systems (GNSS) in areas of large earthquak...
Research on deformation precursors of earthquakes was of immediate interest from the middle to the e...
Research on deformation precursors of earthquakes was of immediate interest from the middle to the e...
International audienceWe investigate how two decades of coseismic deformations affect time series of...
We analyze GNSS data from GEONET data in the vicinity of the 2004 M6.6 Chuetsu and the 2007 M6.6 Chu...
Regional networks of Global Navigation Satellite System (GNSS) stations cover seismically and volcan...
Regional networks of Global Navigation Satellite System (GNSS) stations cover seismically and volcan...
© 2017 Elsevier Ltd Since the 1990s, seismic deformations have been commonly determined using the Gl...
Monitoring of crustal deformation provides essential information for seismology and volcanology. For...
We clarified crustal deformation before and after the 2018 M6.1 northern Osaka earthquake using GNSS...
Analysis of data from permanent GPS observation stations located in tectonically active regions prov...
Studies of GPS data carried out before and after the great Wenchuan earthquake of Ms8.0 on May 12, 2...
We have developed a global earthquake monitoring system based on low‐latency measurements from more ...
Monitoring earthquakes to rapidly forecast their consequences remains a challenging task, especially...
The results of Global Navigational Satellite System (GNSS) observations in the regions of large eart...
The results of observation of Global Navigation Satellite Systems (GNSS) in areas of large earthquak...
Research on deformation precursors of earthquakes was of immediate interest from the middle to the e...
Research on deformation precursors of earthquakes was of immediate interest from the middle to the e...
International audienceWe investigate how two decades of coseismic deformations affect time series of...
We analyze GNSS data from GEONET data in the vicinity of the 2004 M6.6 Chuetsu and the 2007 M6.6 Chu...
Regional networks of Global Navigation Satellite System (GNSS) stations cover seismically and volcan...
Regional networks of Global Navigation Satellite System (GNSS) stations cover seismically and volcan...
© 2017 Elsevier Ltd Since the 1990s, seismic deformations have been commonly determined using the Gl...
Monitoring of crustal deformation provides essential information for seismology and volcanology. For...
We clarified crustal deformation before and after the 2018 M6.1 northern Osaka earthquake using GNSS...
Analysis of data from permanent GPS observation stations located in tectonically active regions prov...
Studies of GPS data carried out before and after the great Wenchuan earthquake of Ms8.0 on May 12, 2...
We have developed a global earthquake monitoring system based on low‐latency measurements from more ...
Monitoring earthquakes to rapidly forecast their consequences remains a challenging task, especially...