Coseismic Deformation Field and Fault Slip Distribution Inversion of the 2020 Jiashi Ms 6.4 Earthquake: Considering the Atmospheric Effect with Sentinel-1 Data Interferometry [PDF]
Sensors, 2023 Due to some limitations associated with the atmospheric residual phase in Sentinel-1 data interferometry during the Jiashi earthquake, the detailed spatial distribution of the line-of-sight (LOS) surface deformation field is still not fully understood ...
Xuedong Zhang +4 more
doaj +2 more sources
Coseismic fault-slip distribution of the 2019 Ridgecrest Mw6.4 and Mw7.1 earthquakes [PDF]
Scientific Reports, 2021 The 2019 Ridgecrest, California seismic sequence, including an Mw6.4 foreshock and Mw7.1 mainshock, represent the largest regional seismic events within the past 20 years.
Yang Gao +6 more
doaj +2 more sources
Identification of Source Mechanisms for the August 5 2018 Mw 6.9 and the August 9 2018 Mw7.0 Lombok Earthquakes [PDF]
Jurnal Penelitian Fisika dan Aplikasinya, 2020 A series of earthquakes with magnitudes ranging from 5.8 to 7.0 occurred in Lombok in the period of July to August 2018. Two events occurred consecutively, the 6.9 on August 5, 2018 (11:46:38 UTC), and the 7.0 on August 9, 2018 (14:56:28 UTC).
Ramadhan Priadi +3 more
doaj +2 more sources
Liquid-Solid Slip on Charged Walls: The Dramatic Impact of Charge Distribution [PDF]
Physical Review Letters, 2020 Main text: 7 pages, 3 figures; supplemental material: 22 pages, 5 figures; to be published in Physical Review ...
Yanbo Xie +3 more
openaire +4 more sources
Adaptive regularization of earthquake slip distribution inversion [PDF]
Tectonophysics, 2016 Abstract Regularization is a routine approach used in earthquake slip distribution inversion to avoid numerically abnormal solutions. To date, most slip inversion studies have imposed uniform regularization on all the fault patches. However, adaptive regularization, where each retrieved parameter is regularized differently, has exhibited better ...
Wang, Chisheng +6 more
openaire +2 more sources
InSAR analysis reveals insights into the Ms 6.2 earthquake rupture and tectonic dynamics of the northeast margin of the Qinghai‒Tibet plateau [PDF]
Scientific ReportsOn 18 December 2023, an Ms 6.2 earthquake occurred in Jishishan County, Linxia Prefecture, Gansu Province, China. As the strongest seismic event in the region since records began, it caused significant casualties and property damage while providing a ...
Guangtong Sun +4 more
doaj +2 more sources
No-slip billiards with particles of variable mass distribution [PDF]
Chaos: An Interdisciplinary Journal of Nonlinear Science, 2022 Astute variations in the geometry of mathematical billiard tables have been and continue to be a source of understanding their wide range of dynamical behaviors, from regular to chaotic. Viewing standard specular billiards in the broader setting of no-slip (or rough) collisions, we show that an equally rich spectrum of dynamics can be called forth by ...
J. Ahmed, C. Cox, B. Wang
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The effect of slip distribution on flow past a circular cylinder
Journal of Fluids and Structures, 2014 A slip boundary has been shown to have a significant impact on flow past bluff bodies. In this work and using a circular cylinder as a model system, the effects of various slip configurations on the passing flow are investigated. A theoretical analysis using matched-asymptotic expansion is first performed in the small-Reynolds number regime following ...
Dandan Li +8 more
openaire +2 more sources
Frontiers in Earth Science, 2022 The 2021 Mw 7.3 Maduo earthquake revealed the significant seismic hazard of faults developed within the Bayan Har Block of eastern Tibet, China (e.g., the Kunlun Pass–Jiangcuo Fault).
Xiaoran Fan +6 more
doaj +1 more source
Seismica, 2023 On February 6, 2023, two large earthquakes occurred near the Turkish town of Kahramanmaraş. The moment magnitude (Mw) 7.8 mainshock ruptured a 310 km-long segment of the left-lateral East Anatolian Fault, propagating through multiple releasing step-overs.
S. Barbot +7 more
semanticscholar +1 more source