Search results for " thrust"

showing 10 items of 59 documents

Sedimentation close to the active Medlicott Wadia Thrust (Western Himalaya): how to estimate climatic base level changes and tectonics.

2017

16 pages; International audience; The Medlicott-Wadia Thrust (MWT) is one of the major active out-of-sequence thrusts in the Himalaya. Studies on Quaternary terraces in its vicinity have been performed using sedimentological, geomorphic and geochronological methods. We focus on the Riasi zone, south of the Pir Panjal range, in the Jammu and Kashmir region of India. The sedimentary units of Quaternary landforms have been mapped as a function of their location with respect to the thrust faults, their relative chronology, and their lithology. Three aggrading sedimentary units, five thin units above strath surfaces at the footwall of the fault system, and seven thin units above strath surfaces …

010504 meteorology & atmospheric sciencesLithologyHimalayaAllostratigraphyFault (geology)010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesStrath terracesPaleontologyAggradationThrust faultOut-of-sequence thrustGeomorphology0105 earth and related environmental sciencesEarth-Surface Processes[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonicsgeographygeography.geographical_feature_category[ SDU.STU.TE ] Sciences of the Universe [physics]/Earth Sciences/Tectonics15. Life on landTectonics[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphySedimentary rockQuaternaryGrowth faultGeologyGrowth fault
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Seismic sources and stress transfer interaction among axial normal faults and external thrust fronts in the Northern Apennines (Italy): A working hyp…

2016

In this study we analyse the main potential seismic sources in some axial and frontal sectors of the Northern Apennines, in Italy. This region was hit by a peculiar series of earthquakes that started in 1916 on the external thrust fronts near Rimini. Later, in 1917-1921, seismicity (up to Mw approximate to 6.5) shifted into the axial zone and clearly migrated north-westward, along the belt of active normal faults. The collection of fault-slip data focused on the active normal faults potentially involved in this earthquake series. The acquired data allowed us to better characterize the geometry and kinematics of the faults. In a few instances, the installation of local seismic networks durin…

010504 meteorology & atmospheric sciencesMagnitude (mathematics)ThrustInduced seismicity010502 geochemistry & geophysicsCluster (spacecraft)01 natural sciencesStress changeStress (mechanics)1916-1920 earthquake cluster0105 earth and related environmental sciencesEarth-Surface ProcessesSeismotectonicsStatic stress transferExternal thrust frontsAxial normal faultSeismic sourcesNorthern ApennineGeophysicsTime space1916–1920 earthquake clusterExternal thrust frontAxial normal faultsSeismic sourceSeismologyGeologyTectonophysics
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Active tectonics along the south east offshore margin of Mt. Etna: New insights from high-resolution seismic profiles

2018

The offshore margin of Mt. Etna has been shaped by Middle Pleistocene to Holocene shortening and extension and, more recently, by gravity-related sliding of the volcanic edifice. These processes have acted contemporaneously although the gravitational component largely prevails over the tectonic one. In order to investigate this issue, we focused on the main role of active tectonics along the south-eastern offshore of Mt. Etna by means of marine high-resolution seismic data. Seismic profiles revealed post-220 ka sedimentary deposits unconformably overlaying the Lower-Middle Pleistocene Etnean clayey substratum and volcanics of the Basal Tholeiitic phase and the Timpe phase. Offshore Aci Trez…

010504 meteorology & atmospheric sciencesPleistoceneSettore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/03 - Geologia Strutturaleactive tectonics010502 geochemistry & geophysics01 natural sciencesSicilian thrust-beltPaleontologyActive tectonicActive tectonics; Ionian Sea; Mt. Etna; Seismic investigation; Sicilian thrust-belt; Earth and Planetary Sciences (all)Seismic investigationHolocene0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryContinental shelfMt. Etnalcsh:QE1-996.5Fold (geology)Ionian SeaMt. Etna; seismic investigation; active tectonics; Sicilian thrust-belt; Ionian SeaSeafloor spreadingVolcanic rocklcsh:GeologyTectonicsGeneral Earth and Planetary SciencesSedimentary rockEarth and Planetary Sciences (all)Geology
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Thermal and structural modeling of the Scillato wedge-top basin source-to-sink system. Insights into the Sicilian fold-and-thrust belt evolution (Ita…

2019

AbstractTemperature-dependent clay mineral assemblages, vitrinite reflectance, and one-dimensional (1-D) thermal and three-dimensional (3-D) geological modeling of a Neogene wedge-top basin in the Sicilian fold-and-thrust belt and its pre-orogenic substratum allowed us to: (1) define the burial history of the sedimentary succession filling the wedge-top basin and its substratum, (2) reconstruct the wedge-top basin geometry, depocenter migration, and sediment provenance through time in the framework of a source-to-sink system, and (3) shed new light into the kinematic evolution of the Apennine-Maghrebian fold-and-thrust belt.The pre-orogenic substratum of the Scillato basin shows an increase…

010504 meteorology & atmospheric sciencesmixed layers illite-smectiteStratigraphyCenozoic deformation[SDU.STU]Sciences of the Universe [physics]/Earth SciencesReflectionStructural basin010502 geochemistry & geophysics01 natural sciencesWedge (geometry)Paleontologywedge-top basin; vitrinite reflectance; mixed layers illite-smectite; thermal modelling; source-to-sink systems; Sicilian fold-and-thrust beltSicilian fold-and-thrust beltThermalthermal modellingClay mineralSedimentologySource to sinkEurope faultsvitrinite reflectancesource-to-sink systems0105 earth and related environmental sciencesMesozoic sedimentary rocks tectonicsgeographygeography.geographical_feature_categoryFaultingGeologySedimentology15. Life on landwedge-top basinlanguage.human_languageStratigraphyFold and thrust beltlanguageThree dimensional computer graphicsSicilianGeologyTertiary
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Late Quaternary coastal uplift of southwestern Sicily, central Mediterranean sea

2021

Abstract Mapping and luminescence aging of raised marine terraces and aeolian ridges along an ∼90 km coastal stretch in southwestern Sicily provide the first quantitative assessment of vertical tectonic deformation in this region, which spans the frontal part of an active thrust belt. We recognized a staircase of eleven terraces and nine related aeolian ridges. The elevation profile of terraces parallel to the coast shows a >90 km long bell-shaped pattern, onto which shorter-wavelength (∼10 km long) undulations are superimposed. Luminescence ages from terraced beach deposits and aeolian sediments constrain the position of paleoshorelines formed during MIS 5e, 7a and 7c, with a maximum uplif…

010506 paleontologyArcheologyMarine terracesEarly Pleistocene010504 meteorology & atmospheric sciencesPleistoceneLuminescence datingSettore GEO/03 - Geologia StrutturaleFold growth01 natural sciencesMarine terracePaleontologyMediterranean seaContinental marginAeolian ridgeEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesGlobal and Planetary ChangegeographyFrontal thrust beltgeography.geographical_feature_categoryThermoluminescence datingBedrockGeologyPleistoceneMediterranean seaAeolian ridgesAeolian processesQuaternaryGeologySouthwestern sicilyQuaternary Science Reviews
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Geodetic and geological evidence of active tectonics in south-western Sicily (Italy)

2014

Abstract Integrated geological, geodetic and marine geophysical data provide evidence of active deformation in south-western Sicily, in an area spatially coincident with the macroseismic zone of the destructive 1968 Belice earthquake sequence. Even though the sequence represents the strongest seismic event recorded in Western Sicily in historical times, focal solutions provided by different authors are inconclusive on possible faulting mechanism, which ranges from thrusting to transpression, and the seismogenic source is still undefined. Interferometric (DInSAR) observations reveal a differential ground motion on a SW–NE alignment between Campobello di Mazara and Castelvetrano (CCA), locate…

Active tectonicsPleistoceneSettore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/03 - Geologia StrutturaleGeodetic datumSicilian fold and thrust belt; Geodesy; Active tectonicsaActive faultTranspressionTectonicsSequence (geology)GeophysicsSeismic hazardThrust faultActive tectonicsaGeologySeismologySicilian fold and thrust beltGeodesyEarth-Surface ProcessesSicilian fold and thrust belt; Geodesy; Active tectonics
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Active deformation in a sector of the Sicilian-Maghrebian Chain: new insights from integrated GNSS, structural high-resolution seismic reflection and…

2016

We document active deformation in a sector of the Sicilian Maghrebian Chain exposed in north Sicily and in its offshore prolongation on the basis of the integrated analysis of 1) time series of data collected by GNSS acquisition representing the change in the positions (X and Y) of permanent stations located in Palermo, Partinico, Prizzi, and Termini compared to the IGS station of Noto, 2) high-resolution (Sparker) single-channel reflection seismic data, 3) structural data, and 4) seismological data. The average values for the velocity vectors obtained for the Palermo, Partinico, Prizzi, and Termini Imerese stations are 4.55, 2.97, 2.96, and 2.15 mm/yr, respectively. The direction of the ve…

Active thrusting Sicilian-Maghrebian chain North Sicily GNSS velocity.Settore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/03 - Geologia Strutturale
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The role of trapped fluids during the development and deformation of a carbonate/shale intra-wedge tectonic mélange (Mt. Massico, Southern Apennines,…

2020

Abstract Numerous studies exist on exhumed tectonic melanges along subduction channels whereas, in accretionary wedge interiors, deformation mechanisms and related fluid circulation in tectonic melanges are still underexplored. We combine structural and microstructural observations with geochemical (stable and clumped isotopes and isotope composition of noble gases in fluid inclusions of calcite veins) and U-Pb geochronological data to define deformation mechanisms and syn-tectonic fluid circulation within the Mt. Massico intra-wedge tectonic melange, located in the inner part of the central-southern Apennines accretionary wedge, Italy. This melange developed by shear deformation at the bas…

CalciteDécollementAccretionary wedge010504 meteorology & atmospheric sciencesSubductionStable and clumped isotopestable and clumped isotopesGeochemistryGeologyCrustMélange010502 geochemistry & geophysicsOverprinting01 natural sciencesFold and thrust beltTectonic mélangechemistry.chemical_compoundNoble gasechemistrytectonic mélange; fluid-rock interaction; stable and clumped isotopes; noble gases; fold and thrust beltnoble gasesFluid inclusionsFluid-rock interactionGeology0105 earth and related environmental sciences
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Numerical investigation of deformation mechanics in fold-and-thrust belts: Influence of rheology of single and multiple décollements

2012

[1] Thin-skinned fold-and-thrust belts related to convergence tectonics develop by scraping off a rock sequence along a weaker basal decollement often formed by water-saturated shale layers or low-viscosity salt horizons. A two-dimensional finite element model with a viscoelastoplastic rheology is used to investigate the structural evolution of fold-and-thrust belts overlying different types of decollements. In addition, the influence of multiple weak layers in the stratigraphic column is studied. Model shale decollements are frictional, with lower friction angles as the cover sequence. Model salt layers behave linear viscous, due to a lower viscosity as the cover sequence, or with a power …

DécollementgeographyAccretionary wedgegeography.geographical_feature_category010504 meteorology & atmospheric sciencesDeformation (mechanics)GeometryFold (geology)GeophysicsImbrication010502 geochemistry & geophysics01 natural sciencesThrust tectonicsTectonicsGeophysicsGeochemistry and PetrologyFold and thrust beltGeology0105 earth and related environmental sciencesTectonics
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A new approach to the design of a speed-torque-controlled rubber V-belt variator

2005

This paper presents a new model for a torque-speed-sensing rubber V-belt variator. The actuators are of the centrifugal roller kind on the driver side and a helical torque cam plus a compression-torsion spring on the driven side. The equations permit designing the actuator geometry in order to keep the transmissible torque as close as possible to the torque request in the whole operative field. Moreover, a procedure is suggested for the most proper design of an automatic variator of this kind. It permits choosing the required variogram of the transmission, i.e. the matching between the engine and the transmission, and designing the actuators: roller mass, housing shape, contact plate angle…

EngineeringTest benchVariatorAutomatic transmissionbusiness.industryMechanical EngineeringAerospace EngineeringTorsion (mechanics)Mechanical engineeringThrustComputer Science::Otherlaw.inventionComputer Science::Roboticslawcontinuously variable transmission rubber V-belt automatic transmission axial thrusts regulation.TorqueActuatorbusinessSimulationContinuously variable transmissionProceedings of the Institution of Mechanical Engineers, Part D: Journal of Automobile Engineering
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