Earthquakes and cluster dynamics during interseismic phases between the Northern and Central Apennines (Italy)

Clicks: 9
ID: 331529
2026
Article Quality & Performance Metrics
Overall Quality
Not rated
Combines reader engagement with the AI quality analysis. This article has not been analysed, so there is no overall score — reader engagement is measured and shown alongside.
AI Quality Assessment
Not analyzed
Readership in this journal
Emerging

Ranked #324 of 338 articles by views in geophysical journal international

Most read Least read

Bar heights use a square-root scale. Only the 120 most-read articles are drawn; the journal has 338 in total.

Mint this article as an NFT
Not yet minted

Create a permanent, verifiable on-chain record of this article on the Scimatic Network. The NFT is held in your Journament account, and you can withdraw it to your own wallet at any time.

5 SUSD one-off · no wallet required
Abstract
Summary In the last thirty years, the Northern and Central Apennines (Italy) have been affected by three main destructive seismic sequences: the 1997 Colfiorito (three events ML > 5.5), the 2009 L’Aquila (one event ML > 5.5), and the 2016–2017 Amatrice-Visso-Norcia (three events ML > 5.5). Several studies have analysed the spatial-temporal evolution and processes driving each sequence, focused more on the foreshock-mainshock-aftershocks dynamics. Here, we focus on the 2018–2024 interseismic period, aiming to unravel the long-term seismogenic behaviour of this region. We first relocated the earthquake catalogue and identified clusters through a declustering algorithm. During this phase, background seismicity and most of the clusters were arranged in a 2-3 km thick low- angle layer. We found that (i) most clusters were driven by an aseismic process, (ii) the depth of both clusters and seismicity layer increased toward the southeast, (iii) the volume of clusters decreases to the southeast, (iv) the low-angle layer almost disappeared in the L’Aquila area. Comparing two interseismic phases (2011–2016 and 2018–2024), we found striking similarities with events occurring on same sites and characterized by both foreshock-mainshock-aftershocks and swarm-like behaviour. In addition to this, the L’Aquila area was seismically more “silent” compared to the norther sites during both interseismic phases. We propose that these different long-term seismogenic behaviours may reflect variation in the structure and rheology of the upper crust moving from the Northern to the Central Apennines. This highlights the important role of the structural inheritance in controlling how the active deformation can affect the interseismic period.
Reference Key
openalex_W7120141685 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors
Journal geophysical journal international
Year 2026
DOI
10.1093/gji/ggag396
URL
Keywords Keywords not found

Citations

No citations found. To add a citation, contact the admin at info@scimatic.org

No comments yet. Be the first to comment on this article.