Search results for "Tectonic inversion"

showing 2 items of 2 documents

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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Basin analysis in the Southern Tethyan margin: Facies sequences, stratal pattern and subsidence history highlight extension-to-inversion processes in…

2018

Abstract In the Mediterranean, the South-Tethys paleomargin experienced polyphased tectonic episodes and paleoenvironmental perturbations during Mesozoic time. The Cretaceous shallow-water carbonate successions of the Panormide platform, outcropping in the northern edge of the Palermo Mountains (NW Sicily), were studied by integrating facies and stratal pattern with backstripping analysis to recognize the tectonics vs. carbonate sedimentation interaction. The features of the Requienid limestone, including geometric configuration, facies sequence, lithological changes and significance of the top-unconformity, highlight that at the end of the Lower Cretaceous the carbonate platform was tecton…

010506 paleontologySettore GEO/02 - Geologia Stratigrafica E SedimentologicaNW SicilyCarbonate platformVertical movementStratigraphyInversion (geology)Geology010502 geochemistry & geophysicsCretaceou01 natural sciencesCretaceousCarbonate platformchemistry.chemical_compoundPaleontologyTectonicschemistryFaciesSedimentary basin analysisCarbonateExtensional tectonicsPositive tectonic inversionGeology0105 earth and related environmental sciencesSedimentary Geology
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