Analysis of two microearthquake swarms in Southeastern Sicily: evidence for active faults?

Two microearthquake swarms occurring in Southeastern Sicily during November 1999 and January 2000 were analysed with respect to their seismotectonic features. Given the low magnitude of the events fault plane solutions for only four major events were computed, which revealed normal fault and inverse...

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Main Authors: A. Ursino, G. Di Grazia, H. Langer, L. Scarfì, S. Gresta
Format: Article
Language:English
Published: Istituto Nazionale di Geofisica e Vulcanologia (INGV) 2001-06-01
Series:Annals of Geophysics
Subjects:
Online Access:http://www.annalsofgeophysics.eu/index.php/annals/article/view/3567
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spelling doaj-6ad6def51af141e2b5f003b4496af80f2020-11-24T21:56:55ZengIstituto Nazionale di Geofisica e Vulcanologia (INGV)Annals of Geophysics1593-52132037-416X2001-06-0144410.4401/ag-3567Analysis of two microearthquake swarms in Southeastern Sicily: evidence for active faults?A. UrsinoG. Di GraziaH. LangerL. ScarfìS. GrestaTwo microearthquake swarms occurring in Southeastern Sicily during November 1999 and January 2000 were analysed with respect to their seismotectonic features. Given the low magnitude of the events fault plane solutions for only four major events were computed, which revealed normal fault and inverse fault mechanisms. From the comparison of waveforms and the relation of P- and S-wave peak amplitudes, two families of multiplets were identified, each representing a distinct type of seismic dislocation. Composite fault plane solutions for the two families showed the same trends as for the single major events. The small number of mismatches of the composite solutions supports the hypothesis of two distinct types of seismic dislocation during the whole sequence, i.e. a normal fault mechanism along E-W striking planes and an inverse fault mechanism along NE-SW striking planes.http://www.annalsofgeophysics.eu/index.php/annals/article/view/3567southeastern Sicilyfocal mechanismsmultlipet eventswavw amplitude ratioscomposite fault plane solution
collection DOAJ
language English
format Article
sources DOAJ
author A. Ursino
G. Di Grazia
H. Langer
L. Scarfì
S. Gresta
spellingShingle A. Ursino
G. Di Grazia
H. Langer
L. Scarfì
S. Gresta
Analysis of two microearthquake swarms in Southeastern Sicily: evidence for active faults?
Annals of Geophysics
southeastern Sicily
focal mechanisms
multlipet events
wavw amplitude ratios
composite fault plane solution
author_facet A. Ursino
G. Di Grazia
H. Langer
L. Scarfì
S. Gresta
author_sort A. Ursino
title Analysis of two microearthquake swarms in Southeastern Sicily: evidence for active faults?
title_short Analysis of two microearthquake swarms in Southeastern Sicily: evidence for active faults?
title_full Analysis of two microearthquake swarms in Southeastern Sicily: evidence for active faults?
title_fullStr Analysis of two microearthquake swarms in Southeastern Sicily: evidence for active faults?
title_full_unstemmed Analysis of two microearthquake swarms in Southeastern Sicily: evidence for active faults?
title_sort analysis of two microearthquake swarms in southeastern sicily: evidence for active faults?
publisher Istituto Nazionale di Geofisica e Vulcanologia (INGV)
series Annals of Geophysics
issn 1593-5213
2037-416X
publishDate 2001-06-01
description Two microearthquake swarms occurring in Southeastern Sicily during November 1999 and January 2000 were analysed with respect to their seismotectonic features. Given the low magnitude of the events fault plane solutions for only four major events were computed, which revealed normal fault and inverse fault mechanisms. From the comparison of waveforms and the relation of P- and S-wave peak amplitudes, two families of multiplets were identified, each representing a distinct type of seismic dislocation. Composite fault plane solutions for the two families showed the same trends as for the single major events. The small number of mismatches of the composite solutions supports the hypothesis of two distinct types of seismic dislocation during the whole sequence, i.e. a normal fault mechanism along E-W striking planes and an inverse fault mechanism along NE-SW striking planes.
topic southeastern Sicily
focal mechanisms
multlipet events
wavw amplitude ratios
composite fault plane solution
url http://www.annalsofgeophysics.eu/index.php/annals/article/view/3567
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AT hlanger analysisoftwomicroearthquakeswarmsinsoutheasternsicilyevidenceforactivefaults
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