Results 11 to 20 of about 5,588,444 (128)
About the aftershocks, the Omori law, and the Utsu formula [PDF]
, 2023 After the main shock of an earthquake, a stream of aftershocks that does not subside for a long time is usually observed. Fusakichi Omori found that the frequency of aftershocks decreases hyperbolically with time. It has recently been observed that Omori'
Klain, Boris +3 more
core +1 more source
The Analysis of the Aftershock Sequences of the Recent Mainshocks in Alaska
Applied Sciences, 2022 The forecasting of the evolution of natural hazards is an important and critical problem in natural sciences and engineering. Earthquake forecasting is one such example and is a difficult task due to the complexity of the occurrence of earthquakes. Since
Mohammadamin Sedghizadeh +1 more
doaj +1 more source
AGU Advances, 2021 Earthquake triggering by seismic waves has been recognized as a phenomenon for nearly 30 years. However, our ability to study dynamic triggering has been limited by our ability to capture the triggering stresses accurately and record the resultant ...
Masatoshi Miyazawa +2 more
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Aftershock Rate Changes at Different Ocean Tide Heights
Frontiers in Earth Science, 2020 The differential probability gain approach is used to estimate quantitatively the change in aftershock rate at various levels of ocean tides relative to the average rate model.
P. N. Shebalin, A. A. Baranov
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Increased earthquake rate prior to mainshocks [PDF]
, 2023 According to the Omori-Utsu law, the rate of aftershocks after a mainshock decays as a power law with an exponent close to 1. This well-established law was intensively used in the past to study and model the statistical properties of earthquakes ...
Ashkenazy, Yosef +3 more
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A spatio-temporal analogue of the Omori-Utsu law of aftershock sequences
, 2021 A spatio-temporal version of the well-known Omori-Utsu law of aftershock sequences is proposed. This 'diffusive Omori-Utsu law' satisfies a nonlinear partial differential equation (PDE). A similarity reduction is obtained that reduces the PDE to an ordinary differential equation (ODE).
openaire +2 more sources
Regional variations in the diffusion of triggered seismicity [PDF]
, 2005 We determine the spatiotemporal characteristics of interearthquake triggering in the International Seismological Centre catalogue on regional and global scales. We pose a null hypothesis of spatially clustered, temporally random seismicity, and determine
Ian G. Main +3 more
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Frontiers in Earth ScienceForeshocks and aftershocks occurred before and after the ML6.8 (Mw7.0) earthquake in eastern Taiwan on 18 September 2022. We explore the epicentral distribution and temporal variations for the mainshock, foreshocks, and aftershocks.
Kou-Cheng Chen +4 more
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Analisis waktu berakhirnya gempabumi susulan dengan menggunakan metode Omori, Mogi I, Mogi II, dan Utsu untuk kejadian gempabumi di Indonesia tahun 2009-2017 [PDF]
, 2018 Indonesia merupakan wilayah yang memiliki tingkat seismisitas yang tinggi karena berada pada wilayah pertemuan tiga lempeng tektonik aktif yang menyebabkan banyaknya zona-zona subduksi dan zona patahan sehingga menjadi sumber terjadinya gempabumi ...
Rohmawati, Tita
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Earth's Future, Volume 14, Issue 8, August 2026.Abstract Statistical earthquake forecasting models, such as the Epidemic‐type Aftershock Sequence (ETAS), embed decades of empirical knowledge and assumptions about earthquake triggering, clustering, and catalog completeness. In contrast, neural spatio‐temporal point process (STPP) models often treat seismicity as generic spatiotemporal data without ...
Weixi Tian +3 more
wiley +1 more source