Search results for " Seismicity"

showing 10 items of 49 documents

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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Probabilistic forecast for Northern New Zealand seismic process: a kernel-based approach

2009

Forecast of earthquakes of a given area of Northern New Zealand is provided. It is based on the assumption that future earthquakes activity may be based on the smoothing of past earthquakes. Therefore, seismic activity is described by an intensity function factorized into kernel functions which depend on time longitude and latitude of events.

Forecast of seismic activity kernel estimator New Zealand seismicitySettore SECS-S/01 - Statistica
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Thermo‐Hydro‐Mechanical Model and Caprock Deformation Explain the Onset of an Ongoing Seismo‐Volcanic Unrest

2021

Acknowledgments The authors are grateful to the Editor, Prof. Ben‐Zion Yehuda, and the reviewers: Prof. Micol Todesco and an anonymous reviewer, whose comments and recommendations have significantly improved the quality of this work. The authors acknowledge the financial support of the Petroleum Technology Development Fund (PTDF) Nigeria for this research. The comparison of our models with monitoring data was made possible by the outstanding efforts of the staff at the INGV‐Osservatorio Vesuviano, who provide weekly information about geophysical parameters at the Campanian volcanoes (http://www.ov.ingv.it/ov/en/bollettini/272-campi-flegrei-bollettini-settimanali.html). The authors are parti…

History010504 meteorology & atmospheric sciencesInduced seismicityTechnology developmentSoftware license01 natural sciencesGeophysicsSpace and Planetary ScienceGeochemistry and PetrologyMonitoring dataCaprockEarth and Planetary Sciences (miscellaneous)Forensic engineeringVolcanic unrest0105 earth and related environmental sciencesJournal of Geophysical Research: Solid Earth
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Seismic Network Evaluation through Simulation: An Application to the Italian National Seismic Network

2011

Abstract A properly organized seismic network is a valuable tool for monitoring seismic zones and assessing seismic hazards. In this paper we propose a new method (seismic network evaluation through simulation, SNES) to evaluate the performance of hypocenter location of a seismic network. The SNES method gives, as a function of magnitude, hypocentral depth, and confidence level, the spatial distribution of the number of active stations in the location procedure and their relative azimuthal gaps, along with confidence intervals in hypocentral parameters. The application of the SNES method also permits evaluation of the magnitude of completeness ( M C ), the background noise levels at the sta…

HypocenterSettore GEO/10 - Geofisica Della Terra Solidaseismic network localization errorMagnitude (mathematics)Seismic noiseInduced seismicityBackground noisePlate tectonicsGeophysicsGeochemistry and PetrologyLithosphereEpicenterSeismologyGeologyBulletin of the Seismological Society of America
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Induced seismicity response of hydraulic fracturing: results of a multidisciplinary monitoring at the Wysin site, Poland

2018

Abstract Shale oil and gas exploitation by hydraulic fracturing experienced a strong development worldwide over the last years, accompanied by a substantial increase of related induced seismicity, either consequence of fracturing or wastewater injection. In Europe, unconventional hydrocarbon resources remain underdeveloped and their exploitation controversial. In UK, fracturing operations were stopped after the Mw 2.3 Blackpool induced earthquake; in Poland, operations were halted in 2017 due to adverse oil market conditions. One of the last operated well at Wysin, Poland, was monitored independently in the framework of the EU project SHEER, through a multidisciplinary system including seis…

Induced seismicityMultidisciplinary monitoringInduced seismicity Multidisciplinary monitoring Unconventional hydrocarbon resources Hydraulic fracturingInduced seismicity Hydraulic fracturing multidisciplinary monitoringUnconventional hydrocarbon resourceslcsh:RQElcsh:Medicinelcsh:QHydraulic fracturinglcsh:Science
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Relationship Between Neotectonics And Fluid Escaping In The Northern Sicilian Continental Margin

2011

New exploration in the marine environments has revealed that the fluid escape structures are often associated with neotectonic elements and are aligned along the same direction. Sometimes is observed the migration of fluid along fault planes to the sea floor as gas venting (Forrest et al., 2005). This paper aims to recognize and to classify the different types of structures associated with fluid seepage, particularly those that develop along alignments coinciding with or parallel to the neotectonic lineaments, in order to assess the interactions between tectonics and fluid circulation. The study area extends, from west to east, from the Gulf of Castellammare to the Gulf of Termini (offshore…

Neotectonics Fluid escape Pockmark Mound SeismicitySettore GEO/03 - Geologia Strutturale
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Including Covariates in the ETAS Model Triggered Seismicity

2020

The paper proposes a stochastic process that improves the assessment of seismic events in space and time, considering a contagion model (branching process) within a regression-like framework to take covariates into account. The proposed approach develops the Forward Likelihood for prediction (FLP) method for estimating the ETAS model, including covariates in the model specification of the epidemic component. A simulation study is carried out for analysing the misspecification model effect under several scenarios. Also an application to the Italian catalogue is reported, together with the reference to the developed R package.

R packageSpecificationSpacetimeComputer scienceStochastic processComponent (UML)CovariateEconometricsStatistics::MethodologyInduced seismicityBranching processSSRN Electronic Journal
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Fluid-triggered earthquake swarms in the Rwenzori region, East African Rift—Evidence for rift initiation

2012

The Rwenzori Mountains are located within the Albertine Rift Valley in western Uganda. To monitor the microseismic activity in the area we have deployed a seismic network of up to 35 stations for a period of about 20 months. The analysis of the recordings revealed several earthquake clusters within a restricted area NE of the mountain block. The clusters form elongated pipes with 1–2 km diameter and vertical extensions of 3–5 km. Most of them are located in 5–16 km depths; however one cluster reaches down to 22 km. Each cluster is composed of a series of single earthquake swarms with durations between a few days and more than a week, interrupted by intervals of inactivity of up to several m…

Remotely triggered earthquakesgeographygeography.geographical_feature_categoryRiftFault (geology)Induced seismicityEarthquake swarmGeophysicsLithosphereEast African RiftSeismologyGeologyRift valleyEarth-Surface Processes
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Crustal Structure of the Seismogenic Volume of the 2010–2014 Pollino (Italy) Seismic Sequence From 3D P- and S-Wave Tomographic Images

2021

A tomographic analysis of Mt. Pollino area (Italy) has been performed using earthquakes recorded in the area during an intense seismic sequence that occurred between 2010 and 2014. 870 local earthquakes with magnitude ranging from 1.8 to 5.0 were selected considering the number of recording stations, the signal quality, and the hypocenter distribution. P- and S-wave arrival times were manually picked and used to compute 3D velocity models through tomographic seismic inversion. The resulting 3D distributions of VP and VS are characterized by high resolution in the central part of the investigated area and from surface to about 10 km below sea level. The aim of the work is to obtain high-qual…

Seismic gapHypocenterseismic gapScienceQseismic sequenceMagnetic dipMagnitude (mathematics)Context (language use)Induced seismicitycrustal structurePollinoTectonicsgeodynamics and seismicitycrustal structure; geodynamics and seismicity; Italian Apennine; Pollino; seismic gap; seismic sequence; velocity tomographyGeneral Earth and Planetary SciencesSeismic inversionItalian Apenninevelocity tomographySeismologyGeologyFrontiers in Earth Science
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Interaction between seismicity and deformation on different time scales in volcanic areas: Campi Flegrei and Stromboli

2019

We study oscillations recorded at Stromboli and Campi Flegrei by different sensors: seismometers, strainmeters and tiltmeters. We examine both the high-frequency (>0.5 Hz) portion of the spectrum and very long period signals up to tidal scales. In this context, seismicity and deformation are investigated on different time scales (from minutes to days/years) in order to identify the basic elements of their interaction, whose understanding should provide new insights on the predictive models. In this work, the strict relation of tides and volcanic processes is shown. At Stromboli, indeed the transition from the stationary phase to the non-stationary phase seems to have a tidal precu…

Seismometer010504 meteorology & atmospheric scienceslcsh:Dynamic and structural geologyanalysisfrequency analysisTiltmeterContext (language use)VolcanismInduced seismicity010502 geochemistry & geophysicsdiurnal variation01 natural sciencesvolcanic eruptionvolcanologylcsh:QE500-639.5lcsh:Science0105 earth and related environmental sciencesgeographyvolcanismgeography.geographical_feature_categoryVulcanian eruptionlcsh:QE1-996.5deformationGeneral MedicineVolcanologydeformation; diurnal variation; frequency analysis; numerical model; seismicity; time series; analysis; volcanic eruption; volcanism;volcanologylcsh:GeologyVolcanolcsh:Qseismicitytime seriesnumerical modelGeologySeismology
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