Results 51 to 60 of about 51,303 (164)
Abstract Many short‐term slow slip events (S‐SSEs) occur at the transition zone along the Nankai subduction zone, southwest Japan. Because crustal deformation due to a single S‐SSE is small, the source fault is often represented using a planar uniform single‐fault slip model, resulting in little constraint on the spatial heterogeneity
Masayuki Kano, Aitaro Kato
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The present study aims at developing a new strategy to model the spatial variability of slip on the rupture plane using multi-dimensional ensemble empirical mode decomposition (MEEMD) technique. Here, the earthquake slip distribution is split into finite
Sangeetha S, Raghukanth S.T.G
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An unusual devastating tsunami occurred on September 28, 2018 after a strike‐slip faulting earthquake in Sulawesi, Indonesia. The induced tsunami struck Palu city with ∼4‐m flow depth.
Tung‐Cheng Ho +8 more
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Stochastic model of heterogeneity in earthquake slip spatial distributions [PDF]
SUMMARY Finite-fault source inversions reveal the spatial complexity of earthquake slip or pre-stress distribution over the fault surface. The basic assumption of this study is that a stochastic model can reproduce the variability in amplitude and the long-range correlation of the spatial slip distribution.
Daniel Lavallée +2 more
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Distribution of seismicity across strike‐slip faults in California [PDF]
The distribution of seismicity about strike‐slip faults provides measurements of fault roughness and damage zone width. In California, seismicity decays with distance from strike‐slip faults according to a power law ∼(1 + x2/d2)−γ/2. This scaling relation holds out to a fault‐normal distance x of 3–6 km and is compatible with a “rough fault loading ...
Peter M. Powers, Thomas H. Jordan
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Distribution of slip at the northern Sumatran fault system [PDF]
We model spatial variations in horizontal displacements of 117 geodetic sites measured during annual surveys in 1989–1996 with the Global Positioning System (GPS) as elastic strain across a locked strike‐slip fault to infer the contemporary slip rate, locking depth, and location of the Sumatran fault (SF) in northern Sumatra (1°S‐3°N). GPS‐derived slip
J. F. Genrich +7 more
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Although the Zhaotong−Ludian fault is a seismically active zone located in the boundary between the Sichuan−Yunnan block and the South China block, it has not experienced a large earthquake greater than Mw 7 since at least 1700.
Yufen Niu +6 more
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Objective On October 24, 2023, an MS 5.5 earthquake occurred in Subei County, Jiuquan City, Gansu Province. The epicenter was located in the Qilian mountain seismic belt at the northeastern margin of the Qinghai-Tibet Plateau.
XIONG Guohua +7 more
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Megathrust earthquakes that occur repeatedly along the plate interface of subduction zones can cause severe damage due to strong ground motion and the destructive tsunamis they can generate.
Masaru Nakano +5 more
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The 2017 Jiuzhaigou earthquake (Ms = 7.0) struck the eastern Tibetan Plateau and caused extensive concern. However, the reported slip models of this earthquake have distinct discrepancies and cannot provide a good fit for GPS data.
Zhengwen Sun, Yingwen Zhao
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