Search results for "Seismic reflection profiles"

showing 3 items of 3 documents

Structural architecture and active deformation pattern in the northern sector of the Aeolian-Tindari-Letojanni fault system (SE Tyrrhenian Sea-NE Sic…

2017

Framed in the current geodynamics of the central Mediterranean, the Aeolian-Tindari-Letojanni fault system is part of a wider NW-SE oriented right-lateral wrench zone which accommodates diverging motion between regional-scale blocks located at the southern edge of the Calabrian Arc. In order to investigate the structural architecture and the active deformation pattern of the northern sector of this tectonic feature, structural observations on-land, high and very-high resolution seismic reflection data, swath bathymetry data and seismological and geodetic data were merged from the Lipari-Vulcano volcanic complex (central sector of the Aeolian Islands) to the Peloritani Mountains across the G…

Settore GEO/02 - Geologia Stratigrafica E Sedimentologica010504 meteorology & atmospheric sciencesSettore GEO/03 - Geologia StrutturaleStructural analysisGPS geodesyInduced seismicityFault (geology)010502 geochemistry & geophysics01 natural sciencesSouthern Tyrrhenian seaNE SicilySouthern Tyrrhenian sea NE Sicily seismic reflection profiles structural analysis seismology GPS geodesyBathymetrySeismology0105 earth and related environmental sciencesgeographySeismic reflection profilesgeography.geographical_feature_categoryGeodetic datumGeologyGeophysicsGeodynamicsTectonicsVolcanoMagmaGeneral Earth and Planetary SciencesSouthern Tyrrhenian sea NE Sicily seismic reflection profiles structural analysis seismology GPS geodesy.SeismologyGeologyItalian Journal of Geosciences
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SIRIPRO PROJECT: DEEP CRUSTAL SETTING IN THE NORTHERN SICILY CONTINENTAL MARGIN AND ITS ADJACENT ONSHORE

2009

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaNORTHERN SICILYSEISMIC REFLECTION PROFILESCRUSTAL SETTING
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An active oblique-contractional belt at the transition between the Southern Apennines and Calabrian Arc: The Amendolara Ridge, Ionian Sea, Italy

2014

High-resolution, single-channel seismic and multibeam bathymetry data collected at the Amendolara Ridge, a key submarine area marking the junction between the Apennine collision belt and the Calabrian subduction forearc, reveal active deformation in a supposedly stable crustal sector. New data, integrated with existing multichannel seismic profiles calibrated with oil-exploratory wells, show that middle to late Pleistocene sediments are deformed in growth folds above blind oblique-reverse faults that bound a regional pop-up. Data analysis indicates that similar to 10 to 20km long banks that top the similar to 80km long, NW-SE trending ridge are structural culminations above en echelon fault…

Settore GEO/02 - Geologia Stratigrafica E Sedimentologicaseismic reflection profilessouthern Italyblind fault segment modelingSettore GEO/03 - Geologia StrutturaleAmendolara Ridge Ionian SeaActive fault-related folds; Blind fault segment modeling; Ionian basin; Seismic reflection profiles; Southern italyactive fault-related foldsIonian Basin
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