Results 31 to 40 of about 594,765 (205)
Megathrust earthquakes impose changes of differential stress and pore pressure in the lithosphere-asthenosphere system that are transiently relaxed during the postseismic period primarily due to afterslip, viscoelastic and poroelastic processes. Especially during the early postseismic phase, however, the relative contribution of these processes to the ...
Peña, Carlos +14 more
openaire +7 more sources
Co- and Postseismic Deformation of the 2020 Mw 6.3 Nima (Tibet, China) Earthquake Revealed by InSAR Observations [PDF]
On 22 July 2020, an Mw 6.3 earthquake occurred in Nima County, central Qinghai-Tibet Plateau, China. We used the synthetic aperture radar interferometry (InSAR) technique with Sentinel-1 images to retrieve the line of sight (LOS) coseismic deformation ...
Miaomiao Zhang +8 more
doaj +2 more sources
The study of postseismic deformation is important for constraining the viscoelastic properties of the Earth and inverting the post-earthquake process. The levelling survey revealed that the area near Beichuan elevated 5.3 cm about two years after the MW7.
Feng Li +3 more
doaj +1 more source
The 2011 Tohoku-oki earthquake produced the most well-recorded postseismic deformation of any megathrust earthquake in the world. Over the last decade, researchers have used a dense and widespread geodetic network of more than 1300 Global Navigation ...
Sambuddha Dhar +3 more
doaj +1 more source
Surface displacements associated with earthquake-cycle deformation of active faults significantly influence the accuracy of geodetic datum and reference frames, especially for the Taiwan area with high plate convergence and deformation rates.
Kwo-Hwa Chen +2 more
doaj +1 more source
The Palu MW7.4 earthquake occurred on September 28, 2018, with the epicenter at 119.86°, 0.72°. The severe shaking caused severe damage in Central Sulawesi, especially in Palu.
Irma Yusiyanti +3 more
doaj +1 more source
Spatiotemporal functional modeling of postseismic deformations after the 2011 Tohoku-Oki earthquake [PDF]
Abstract Postseismic deformations continue to occur for a long period after major earthquakes. Temporal changes in postseismic deformations can be approximated using simple functions. Since the 2011 Tohoku-Oki earthquake, operating global navigation satellite system stations have been continuously accumulating a remarkable amount of ...
Satoshi Fujiwara +2 more
openaire +3 more sources
The coseismic and postseismic effects are crucial elements in analyzing fault interactions and the regional seismic risk. In this paper, we developed a three-dimensional viscoelastic finite element code to simulate the coseismic and postseismic ...
SUN Yunqiang, LUO Gang, HUANG Luyuan
doaj +1 more source
Dataset_for_Decadal Viscoelastic Postseismic Deformation of the 1964 Mw9.2 Alaska Earthquake
Dataset for the manuscript (No.2020JB019649R) submitted to JGR: solid earth: Decadal Viscoelastic Postseismic Deformation of the 1964 Mw9.2 Alaska ...
Huang, K (via Mendeley Data) +1 more
core +2 more sources
Coseismic and postseismic fault slip characteristics of the 2020 MW6.3 Nima earthquake
The 2020 MW6.3 Nima earthquake occurred in the northern Yibug Caka graben on the Qiangtang Block of the Tibetan Plateau. The epicentral area has complex geological structures, topography, and geomorphology, and there are few near-field ground observation
Yang Liu +3 more
doaj +1 more source

