0000000000465778

AUTHOR

Danilo Cavallaro

0000-0001-9173-3725

showing 5 related works from this author

Evidence of positive tectonic inversion in the north-central sector of the Sicily Channel (Central Mediterranean)

2016

In order to unravel the tectonic evolution of the north-central sector of the Sicily Channel (Central Mediterranean), a seismo-stratigraphic analysis of single- and multi-channel seismic reflection profiles has been carried out. This allowed to identify, between 20 and 50 km offshore the central-southern coast of Sicily, a ~80-km-long deformation belt, characterized by a set of WNW–ESE to NW–SE fault segments showing a poly-phasic activity. Within this belt, we observed: i) Miocene normal faults reactivated during Zanclean–Piacenzian time by dextral strike-slip motion, as a consequence of the Africa–Europe convergence; ii) releasing and restraining bend geometries forming well-developed pul…

Atmospheric SciencePiacenzian010504 meteorology & atmospheric sciencesSicily ChannelSettore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/03 - Geologia StrutturaleInversion (geology)Structural basin010502 geochemistry & geophysics01 natural sciencesNappePush-up structureCompressive featuresEarth and Planetary Sciences (miscellaneous)Tectonic inversionForeland basinStrike-slip motion0105 earth and related environmental sciencesWater Science and TechnologyAnticlinePush-up structuresCompressive featureTectonicsSinistral and dextralCompressive features; Push-up structures; Seismic stratigraphy; Sicily Channel; Strike-slip motion; Tectonic inversion; Water Science and Technology; Atmospheric Science; Earth and Planetary Sciences (miscellaneous)SeismologyGeologySeismic stratigraphy
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Tidal notches, coastal landforms and relative sea-level changes during the Late Quaternary at Ustica Island (Tyrrhenian Sea, Italy)

2017

In this paper we present and discuss data concerning the morphostructural evolution at Ustica Island (Tyrrhenian Sea, Italy) during Late Quaternary. New insights on the relative sea-level changes of Ustica are coming from data collected during a geomorphological field survey around the island, together with the bathymetric analysis of the surrounding seabed and 14C datings on samples of speleothems, flowstones and marine shells found inside three selected sea caves. The survey was mainly accomplished on June 2015 through the first complete snorkel investigation off the about 18 km-long volcanic coast of the island, which allowed to precisely define location, relationship and morphometric fe…

Mediterranean Sea; Sea caves; Tectonic uplift; Ustica; Volcanic geomorphology; Earth-Surface ProcessesTectonic upliftPillow lava010504 meteorology & atmospheric sciencesSettore GEO/04 - Geografia Fisica E GeomorfologiaUstica;Volcanic geomorphology;Tectonic uplift;Mediterranean Sea;Sea caves010502 geochemistry & geophysics01 natural scienceslaw.inventionPaleontologyTectonic upliftMediterranean seaCavelawVolcanic geomorphology; Tectonic uplift; Sea caves; Ustica; Mediterranean SeaMediterranean SeaSea caveRadiocarbon datingSea levelSea caves0105 earth and related environmental sciencesEarth-Surface Processesgeographygeography.geographical_feature_categoryVolcanic geomorphology Tectonic uplift Sea caves Ustica Mediterranean SeaVolcanic geomorphology Tectonic upliftVolcanic rockOceanographyUsticaVolcanic geomorphologyQuaternaryGeology
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Seismic moment tensors and regional stress in the area of the December 2013–January 2014, Matese earthquake sequence (Italy)

2014

Abstract The main goal of this study is to provide moment tensor solutions for small and moderate earthquakes of the Matese seismic sequence in southern Italy for the period of December 2013–January 2014. We estimate the focal mechanisms of 31 earthquakes with local magnitudes related to the Matese earthquake seismic sequence (December 2013–January 2014) in Southern-Central Italy which are recorded by the broadband stations of the Italian National Seismic Network and the Mediterranean Very Broadband Seismographic Network (MedNet) run by the Istituto Nazionale di Geofisica e Vulcanologia (INGV). The solutions show that normal faulting is the prevailing style of seismic deformation in agreeme…

Stress (mechanics)TectonicsSequence (geology)GeophysicsDeformation (mechanics)Moment tensorSeismic momentStress inversionSeismologyGeologyEarth-Surface ProcessesJournal of Geodynamics
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The marine activities performed within the TOMO-ETNA experiment

2016

<p>The TOMO-ETNA experiment was planned in order to obtain a detailed geological and structural model of the continental and oceanic crust beneath Mt. Etna volcano and northeastern Sicily up to the Aeolian Islands (southern Italy), by integrating data from active and passive refraction and reflection seismic methodologies, magnetic and gravity surveys. This paper focuses on the marine activities performed within the experiment, which have been carried out in the Ionian and Tyrrhenian Seas, during three multidisciplinary oceanographic cruises, involving three research vessels (“Sarmiento de Gamboa”, “Galatea” and “Aegaeo”) belonging to different countries and institutions. During the o…

0301 basic medicineSeismometerlcsh:QC851-999010502 geochemistry & geophysicsRemotely operated vehicle01 natural sciencesSonarGravity anomalyEtna offshore; Ionian and Tyrrhenian Seas; Marine geophysical data acquisition; Scientific cruise report; Geophysics03 medical and health sciencesSeismic refraction0105 earth and related environmental sciencesMarine geophysical data acquisitionIonian and Tyrrhenian Seaslcsh:QC801-809Ionian and Tyrrhenian SeaSeafloor spreadinglcsh:Geophysics. Cosmic physics030104 developmental biologyGeophysicsSeismic tomographyScientific cruise reportEtna offshorelcsh:Meteorology. ClimatologySubmarine pipelineGeologySeismologyAnnals of Geophysics
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Coseismic Damage at an Archaeological Site in Sicily, Italy: Evidence of Roman Age Earthquake Surface Faulting

2018

Archaeoseismology can provide a useful chronological tool for constraining earthquakes and documenting significant evidence that would otherwise be lost. In this paper, we report a case of surface faulting on ancient man-made structures belonging to the archaeological site of Santa Venera al Pozzo situated along the eastern flank of Mt. Etna volcano in eastern Sicily (southern Italy), which is affected by well-developed tectonic faults. Geological surveys highlight a set of fractures affecting the archaeological ruins, suggesting the occurrence of a capable fault zone across the area. An integrated geophysical survey was carried out in order to identify the main subsurface tectonic disconti…

Geophysical investigation Archaeoseismological analysis Surface faulting Santa Venera al Pozzo Etna volcano010504 meteorology & atmospheric sciences010502 geochemistry & geophysics01 natural sciencesArchaeologyTectonicsGeophysicsDiscontinuity (geotechnical engineering)Etna volcanoGeochemistry and PetrologySettore GEO/11 - Geofisica ApplicataSeismic refractionElectrical resistivity tomographyRoman ageGeology0105 earth and related environmental sciencesArchaeoseismology
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