Results 51 to 60 of about 5,848,790 (129)
Abstract The spatial distribution of seismicity in active fault zones depends primarily on the geometry of the fault networks. However, recent advances suggest that seismic activity may also be controlled by the rheology of the geological units surrounding fault zones. In the present work, we use seismological and geological analyses to investigate the
Maxime Godano +9 more
wiley +1 more source
On two approaches to studying the aftershocks of a strong earthquake [PDF]
The paper is devoted to comparing two approaches to the study of aftershocks. The methodological foundations of the traditional approach were laid many years ago. A new approach has emerged relatively recently.
Guglielmi, A. V.
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Statistical Characteristics of Seismicity Correlated With Crustal Fluids in the Noto Region
Abstract Earthquake swarms and strong shocks have frequently occurred in Noto Peninsula, Japan, for decades, resulting in a seismicity pattern characterized by a mixture of background earthquakes, swarms, and foreshock/aftershock sequences. Using an improved version of the space‐time Epidemic‐Type Aftershock Sequence model, we extract statistical ...
Yicun Guo +3 more
wiley +1 more source
The Role of Co‐Seismic Devolatilization in Driving Aftershock Sequences in Greece
Abstract We investigate the role of co‐seismic devolatilization in driving aftershock sequences, focusing on three recent sequences in Greece: Thiva, Damasi, and Florina. We use a numerical model incorporating non‐linear diffusion with a source term that accounts for fluid generation via thermal decomposition of carbonates.
Gaëlle Toussaint +3 more
wiley +1 more source
Has happen earthquake earth tectonics with magnitude 6.8 SR in Regency South Manokwari , West Papua Province on April 21, 2012. Purpose from study This is compare four decay models earthquake continuation namely the Omori , Mogi I, Mogi II and models ...
Kristian Enggar Pamuji +4 more
core +1 more source
Method for processing and analyzing tectonic earthquake aftershocks: A new look at old problem [PDF]
The deactivation coefficient has been introduced for the source that cools down after the mainshock of the earthquake. The deactivation coefficient satisfies two conditions.
Guglielmi, A. V.
core +1 more source
Penentuan Asumsi Waktu Berakhirnya Gempa Susulan Studi Kasus Gempabumi Lombok 5 Agustus 2018 [PDF]
Indonesia is located at the meeting point of three active tectonic plates. The consequence is the country is very prone to earthquake disaster, one of the most devastated events is Lombok earthquake occurred on 5 August 2018.
Vellicia, Audrey +2 more
core +1 more source
Ley de Omori para sismos premonitorios y réplicas ocurridos en el valle de Atrato: sismo de Murindó-Antioquia 1992 [PDF]
Los terremotos son fenómenos naturales que ocurren por el movimiento de placas tectónicas y se dividen en varias fases de ocurrencia. En este estudio nos enfocaremos en la fase post-sísmica.
Manjarrés Aarón, Marianella
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Aftershocks following crash of currency exchange rate: The case of RUB/USD in 2014
© CopyrightEPLA, 2018. The dynamical behavior of the currency exchange rate after its large-scale catastrophe is discussed through a case study of the rate of Russian rubles to US dollars after its crash in 2014.
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Natural seismicity is characterized by empirical laws such as the Gutenberg-Richter law and the Omori-Utsu law. The latter is a typical example for the spatio-temporal clustering of seismicity arising from triggering processes related to static and/or ...
Stanchits, Sergei A. +6 more
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