Analysis of Volcanic Seismicity Clustering Using Data of the 2006 Eruption of Alaska's Augustine Volcano

The paper is devoted to the analysis of spatiotemporal grouping of volcanic seismicity events confined to the Augustine volcano in Alaska. Heterogeneity of the seismic regime in the final preparation stage of the 2006 eruption was revealed relative to the regimes during periods of calm and the initial stage of seismic activation. This final stage is presumably associated with the process of magma intrusion into the dike, upon completion of which the eruption began. A detailed analysis of the seismicity of this phase revealed two seismic regimes that differ in their main characteristics. One of the regimes is similar in parameters to that observed at the early preparation stage – a high value of the magnitude-frequency distribution slope parameter ( -value) and a low degree of clustering. The second has a lower b-value and represents a series of clusters ending with the strongest event in the series, followed by a lull.

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Publication Details

Journal
Rossijskij žurnal nauk o zemle/Russian journal of earth sciences
Published
2025-06-20
DOI
https://doi.org/10.2205/2025es001025
Primary Topic
earthquake and tectonic studies
Type
article
Field-Weighted Citation Impact
0.00
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article

Analysis of Volcanic Seismicity Clustering Using Data of the 2006 Eruption of Alaska's Augustine Volcano

П. Н. Шебалин, Е. M. Grekov
Rossijskij žurnal nauk o zemle/Russian journal of earth sciences
earthquake and tectonic studies
article

Analysis of Volcanic Seismicity Clustering Using Data of the 2006 Eruption of Alaska's Augustine Volcano

П. Н. Шебалин, Е. M. Grekov
article en

Abstract

The paper is devoted to the analysis of spatiotemporal grouping of volcanic seismicity events confined to the Augustine volcano in Alaska. Heterogeneity of the seismic regime in the final preparation stage of the 2006 eruption was revealed relative to the regimes during periods of calm and the initial stage of seismic activation. This final stage is presumably associated with the process of magma intrusion into the dike, upon completion of which the eruption began. A detailed analysis of the seismicity of this phase revealed two seismic regimes that differ in their main characteristics. One of the regimes is similar in parameters to that observed at the early preparation stage – a high value of the magnitude-frequency distribution slope parameter ( -value) and a low degree of clustering. The second has a lower b-value and represents a series of clusters ending with the strongest event in the series, followed by a lull.

Rossijskij žurnal nauk o zemle/Russian journal of earth sciences
Lomonosov Moscow State University (RU), Moscow State University (TJ)
Openalex Percentile: Top 82%
earthquake and tectonic studies
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