Results 51 to 60 of about 6,894 (231)

Comparing foreshock characteristics and foreshock forecasting in observed and simulated earthquake catalogs [PDF]

open access: yesJournal of Geophysical Research: Solid Earth, 2014
AbstractIn this paper, we compare the empirical results regarding foreshocks obtained from the Japan data with results for synthetic catalogs in order to clarify whether or not the corresponding results are consistent with the description of the seismicity by a superposition of background activity and epidemic‐type aftershock sequence (ETAS) models ...
Yosihiko Ogata, Koichi Katsura
openaire   +1 more source

Rare Occurrences of Non‐cascading Foreshock Activity in Southern California

open access: yesGeophysical Research Letters, 2021
Earthquakes preceding large events are commonly referred to as foreshocks. They are often considered as precursory phenomena reflecting the nucleation process of the main rupture.
L. Moutote   +3 more
semanticscholar   +1 more source

Are Foreshocks Fore‐Shocks?

open access: yesJournal of Geophysical Research: Solid Earth
AbstractForeshocks are spatially clustered seismic events preceding large earthquakes. Since the dawn of seismology, their occurrence has been identified as a possible mechanism leading to further crustal destabilization, hence, to major failures. However, several cases occurred without any previous anomalous seismic activity, so that the hypothesis of
Davide Zaccagnino   +4 more
openaire   +5 more sources

Foreshock–mainshock–aftershock sequence analysis of the 14 January 2021 (Mw 6.2) Mamuju–Majene (West Sulawesi, Indonesia) earthquake

open access: yesEarth, Planets and Space, 2021
We present here an analysis of the destructive Mw 6.2 earthquake sequence that took place on 14 January 2021 in Mamuju–Majene, West Sulawesi, Indonesia.
P. Supendi   +18 more
semanticscholar   +1 more source

Occurrence rate of ultra-low frequency waves in the foreshock of Mercury increases with heliocentric distance

open access: yesNature Communications, 2021
Studies of Mercury’s foreshock have analyzed in detail the properties of ultra-low frequency waves. However, an open question remains in regards to understanding favorable conditions for these planetary foreshocks waves. Here, we report that 0.05–0.41 Hz
N. Romanelli, G. DiBraccio
semanticscholar   +1 more source

Recognizing the waveform of a foreshock [PDF]

open access: yes, 2020
Abstract The 2011 Mw9.1 Tohoku, Japan, earthquake is the paradigmatic example of an earthquake anticipated by a significant foreshock activity, with a Mw7.3 earthquake occurred two days before, within about 10 km 1. Recent results 2 show that statistically relevant changes can be found in the magnitude distribution after the Mw7.3 foreshock but
Eugenio Lippiello   +2 more
openaire   +1 more source

Real-Time Foreshock–Aftershock–Swarm Discrimination During the 2025 Seismic Crisis near Santorini Volcano, Greece: Earthquake Statistics and Complex Networks

open access: yesGéosciences
The advanced determination of the type (foreshock–aftershock–swarm) of an ongoing seismic cluster is quite challenging; only retrospective solutions have thus far been proposed.
I. Triantafyllou   +3 more
semanticscholar   +1 more source

Oblique propagation and temperature effects on the resonant right-hand ion beam instability

open access: yesFrontiers in Astronomy and Space Sciences, 2023
The resonant right-hand instability (RHI) is often the dominant mode driven by reflected ions upstream of Earth’s quasi-parallel bow shock. In the tradition of Peter Gary, this paper further explores the right-hand instability using numerical solutions ...
Ari Le   +4 more
doaj   +1 more source

Huge July 2025 Kamchatka earthquake followed unusually productive foreshock sequence

open access: yesTemblor
A large foreshock that struck 10 days before the magnitude 8.8 Kamchatka earthquake brought the epicentral megathrust patch closer to failure and produced an exceptionally abundant burst of aftershocks.
R. Stein   +4 more
semanticscholar   +1 more source

Seismogenic structure behaviour revealed by spatial clustering of seismicity in the Umbria-Marche Region (Central Italy)

open access: yesAnnals of Geophysics, 1998
Time variations in the spatial distribution of earthquake epicentres are analyzed by application of the fractal correlation dimension method. The zone under investigation is located in Central Italy, bounded in longitude by 12.0 and 14.4 degrees east and
P. Tosi
doaj   +1 more source

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