2022
DOI: 10.1007/s10712-022-09698-0
|View full text |Cite
|
Sign up to set email alerts
|

Modeling and Prediction of Aftershock Activity

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1

Citation Types

0
13
0

Year Published

2022
2022
2024
2024

Publication Types

Select...
8

Relationship

2
6

Authors

Journals

citations
Cited by 17 publications
(13 citation statements)
references
References 165 publications
0
13
0
Order By: Relevance
“…This allows to obtain the estimate of the parameter b a for all the data regardless of the level of watering of the rock environment. This estimate is necessary during the assessment of post-seismic danger, for example, during the calculation of the parameters of the dynamic Bath's law [Baranov et al, 2022;Motorin and Baranov, 2022].…”
Section: Discussionmentioning
confidence: 99%
See 1 more Smart Citation
“…This allows to obtain the estimate of the parameter b a for all the data regardless of the level of watering of the rock environment. This estimate is necessary during the assessment of post-seismic danger, for example, during the calculation of the parameters of the dynamic Bath's law [Baranov et al, 2022;Motorin and Baranov, 2022].…”
Section: Discussionmentioning
confidence: 99%
“…Post-seismic activity is described by three laws of statistical seismology: Gutenberg -Richter [Gutenberg and Richter, 1944], Omori -Utsu [Utsu et al, 1995], and earthquake productivity [Baranov et al, 2022;Shebalin et al, 2020]. The Gutenberg -Richter law specifies the distribution of magnitudes.…”
Section: Introductionmentioning
confidence: 99%
“…The model described in this article is applicable as a reference model in testing models of the first aftershocks. The case-study of the reference model application in the assessment of a strong aftershock magnitude and the hazardous period duration is presented in [29].…”
Section: Practical Usementioning
confidence: 99%
“…Some authors have tried to give a generalized form of this law in the form of a differential equation and introduced the idea of a "cool down" process after the mainshock [14,15]. In the end, the goal has been to characterize the behavior of aftershocks so the general activity can be predicted after a big event and therefore, asses the risk in a given zone [16]. In addition, there seems to be a relationship between the parameter b of Gutenberg-Richter and the parameter p of Omori which governs the speed of the aftershock's decay [17][18][19][20].…”
Section: Introductionmentioning
confidence: 99%