Search results for "Aftershock"

showing 8 items of 8 documents

Simultaneous seismic wave clustering and registration

2012

In this paper we introduce a simple procedure to identify clusters of multivariate waveforms based on a simultaneous assignation and alignment procedure. This approach is aimed at the identification of clusters of earthquakes, assuming that similarities between seismic events with respect to hypocentral parameters and focal mechanism correspond to similarities between waveforms of events. Therefore we define a distance measure between seismic curves in R^d d>=1, in order to interpret and better understand the main features of the generating seismic process.

Focal mechanismMultivariate statisticsComputer sciencebusiness.industryFunctional clusteringCurve registration Waveform Palermo aftershocks sequenceProcess (computing)Pattern recognitionMeasure (mathematics)Seismic wavePhysics::GeophysicsIdentification (information)WaveformArtificial intelligenceComputers in Earth SciencesCluster analysisbusinessSettore SECS-S/01 - StatisticaSeismologyInformation Systems
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The Palermo (Sicily) seismic cluster of September 2002, in the seismotectonic framework of the Tyrrhenian Sea-Sicily border area

2009

The northern coast of Sicily and its offshore area represent a hinge zone between a sector of the Tyrrhenian
 Basin, characterized by the strongest crustal thinning, and the sector of the Sicilian belt which has emerged. This
 hinge zone is part of a wider W-E trending right-lateral shear zone, which has been affecting the Maghrebian
 Chain units since the Pliocene. Seismological and structural data have been used to evaluate the seismotectonic
 behavior of the area investigated here. Seismological analysis was performed on a data set of about 2100 seismic
 events which occurred between January 1988 and October 2002 in the Southern Tyrrhenian Sea. This paper
 focuses…

Focal mechanismSeismotectonicslcsh:QC801-809CrustInduced seismicityNorthwestern Sicilylcsh:QC851-999seismotectoniclcsh:Geophysics. Cosmic physicsGeophysicsShear (geology)LithosphereSouthern Tyrrhenian Seaseismotectonicslcsh:Meteorology. ClimatologyShear zoneAftershockSeismologyGeologyAnnals of Geophysics
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Effect of Local Geology on Ground Motion in the City of Palermo, Italy, as Inferred from Aftershocks of the 6 September 2002 Mw 5.9 Earthquake

2005

On 6 September 2002 a M w 5.9 earthquake occurred in the southern Tyrrhenian sea, 40 km off the coast of Palermo (Italy). In the days after the mainshock, eight temporary stations were installed in the city to record aftershocks on different geological formations. Seismograms of about 30 earthquakes with magnitude ≥2.8 are analyzed. The data analysis confirms the role of near-surface geology in causing locally significant variations of the ground-shaking level as already inferred by Guidoboni et al. (2003) from historical damage scenario studies. The largest spectral variations estimated through aftershock recordings result in a factor of 10 difference between stiff and soft sites, in frequ…

Geographic information systembusiness.industryAmbient noise levelBoreholeMagnitude (mathematics)GeophysicsAmplitudePalermo site effects EC8Geochemistry and PetrologyNatural hazardbusinessSeismogramGeologySeismologyAftershockBulletin of the Seismological Society of America
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Fragmentation dynamics within shear bands--a model for aging tectonic faults?

2001

A numerical model for packing of fragmenting blocks in a shear band is introduced, and its dynamics is compared with that of a tectonic fault. The shear band undergoes a slow aging process in which the blocks are being grinded by the shear motion and the compression. The dynamics of the model have the same statistical characteristics as the seismic activity in faults. The characteristic magnitude distribution of earthquakes appears to result from frictional slips at small and medium magnitudes, and from fragmentation of blocks at the largest magnitudes. Aftershocks to large-magnitude earthquakes are local recombinations of the fragments before they reach a new quasi-static equilibrium. The …

Magnitude distributionSeismic gapBiophysicsSurfaces and InterfacesGeneral ChemistryPhysics::GeophysicsTectonicsShear (geology)Heat fluxGeneral Materials Science2008 California earthquake studyShear bandAftershockGeologySeismologyBiotechnologyThe European Physical Journal E
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Southern-Tyrrhenian seismicity in space-time-magnitude domain

2006

An analysis is conducted on a catalogue containing more than 2000 seismic events
 occurred in the southern Tyrrhenian Sea between 1988 and October 2002, as an attempt
 to characterise the main seismogenetic processes active in the area in space, time and magnitude domain by means of the parameters of phenomenological laws.
 
 We chose to adopt simple phenomenological models, since the low number of data did
 not allow to use more complex laws.
 
 The two main seismogenetic volumes present in the area were considered for the purpose
 of this work. The first includes a nearly homogeneous distribution of hypocentres in a
 NW steeply dipping layer as far as a…

Southern-Tyrrhenian SeaPlane (geometry)Space timelcsh:QC801-809Magnitude (mathematics)Southern-Tyrrhenian Sea statistical models aftershock sequences background seismicitystatistical modelslcsh:QC851-999Induced seismicityHomogeneous distributionDomain (mathematical analysis)lcsh:Geophysics. Cosmic physicsGeophysicsaftershock sequencesLithosphereSlablcsh:Meteorology. ClimatologySeismologyGeologybackground seismicity.Annals of Geophysics
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Mixed Non-Parametric and Parametric Estimation Techniques in R Package etasFLP for Earthquakes’ Description

2017

etasFLP is an R package which fits an epidemic type aftershock sequence (ETAS) model to an earthquake catalog; non-parametric background seismicity can be estimated through a forward predictive likelihood approach, while parametric components of triggered seismicity are estimated through maximum likelihood; estimation steps are alternated until convergence is obtained and for each event the probability of being a background event is estimated. The package includes options which allow its wide use. Methods for plot, summary and profile are defined for the main output class object. The paper provides examples of the package's use with description of the underlying R and Fortran routines.

Statistics and ProbabilityEarthquakeComputer scienceFortranFortranInduced seismicity010502 geochemistry & geophysicscomputer.software_genre01 natural sciencesPlot (graphics)Point processPhysics::GeophysicsPoint proce010104 statistics & probabilityetasFLP; R; Fortran; point process; ETAS; earthquakesETAS0101 mathematicsearthquakeslcsh:Statisticslcsh:HA1-4737AftershockEtasFLPpoint process0105 earth and related environmental sciencesEvent (probability theory)Parametric statisticscomputer.programming_languageNonparametric statisticsRetasFLP R Fortran point process ETAS earthquakes.Data miningStatistics Probability and UncertaintySettore SECS-S/01 - StatisticacomputerAlgorithmSoftware
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Windowed Etas Models With Application To The Chilean Seismic Catalogs

2015

Abstract The seismicity in Chile is estimated using an ETAS (Epidemic Type Aftershock sequences) space–time point process through a semi-parametric technique to account for the estimation of parametric and nonparametric components simultaneously. The two components account for triggered and background seismicity respectively, and are estimated by alternating a ML estimation for the parametric part and a forward predictive likelihood technique for the nonparametric one. Given the geographic and seismological characteristics of Chile, the sensitivity of the technique with respect to different geographical areas is examined in overlapping successive windows with varying latitude. A different b…

Statistics and ProbabilityNonparametric statisticsManagement Monitoring Policy and LawInduced seismicityGeodesyPoint processPhysics::GeophysicsLatitudeSpace-time point processes ETAS model etasFLP R packagePredictive likelihoodStatisticsSensitivity (control systems)Computers in Earth SciencesAftershockGeologyParametric statistics
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ETAS Space–Time Modeling of Chile Triggered Seismicity Using Covariates: Some Preliminary Results

2021

Chilean seismic activity is one of the strongest in the world. As already shown in previous papers, seismic activity can be usefully described by a space–time branching process, such as the ETAS (Epidemic Type Aftershock Sequences) model, which is a semiparametric model with a large time-scale component for the background seismicity and a small time-scale component for the triggered seismicity. The use of covariates can improve the description of triggered seismicity in the ETAS model, so in this paper, we study the Chilean seismicity separately for the North and South area, using some GPS-related data observed together with ordinary catalog data. Our results show evidence that the use of s…

Technologymodel selectionQH301-705.5QC1-999Induced seismicityPhysics::Geophysicssemiparametric modelComponent (UML)CovariateGeneral Materials Sciencetriggered seismicityBiology (General)InstrumentationQD1-999AftershockBranching processFluid Flow and Transfer ProcessesProcess Chemistry and TechnologySpace timeModel selectionTPhysicsGeneral EngineeringcovariatesEngineering (General). Civil engineering (General)Computer Science ApplicationsSemiparametric modelETAS modelChemistrycovariatesemiparametric modelsTA1-2040GeologySeismologyApplied Sciences
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