Search results for "Fold growth"

showing 3 items of 3 documents

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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Growth pattern of underlithified strata during thrust-related folding

2004

Abstract Asymmetric anticlines with overturned or steeply dipping forelimbs and gently dipping backlimbs are generally interpreted as thrust-related folds. Fold asymmetry occurs as a consequence of forelimb rotation. If deformation takes place in environments dominated by submarine sedimentation, the limbs coincide with the slope (depositional surface) and rotation reflects slope steepening. If folds are nucleated in poorly or unlithified deposits, growth geometry also depends on the properties of the media, such as cohesion and the angle of internal friction. For cohesionless deposits, the tilting of the slope influences the equilibrium of the soft sediments, resulting in gravity-driven fl…

Sedimentary depositional environmentBeddingCompactionAnticlineGeologyFold (geology)NeogenePetrologyLithificationGeomorphologyGeologySoft-sediment deformations Stratal pattern Fold growth Thrust tectonics Pliocene SicilyThrust tectonics
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Multi-temporal tectonic evolution of Capo Granitola and Sciacca foreland transcurrent faults (Sicily channel)

2019

Highlights • Seismic reflection profiles evidence tectonic inversion and active strike-slip faults offshore SW Sicily foreland • Pliocene-Quaternary transpressional inversion of Late Miocene extensional basins • Transpressional fold growth rates were high in Latest Miocene-Pliocene and decreased during Quaternary Joint analysis of high-penetration multi-channel and high-resolution single-channel seismic reflection profiles, calibrated by deep well boreholes, allowed a detailed reconstruction of the Late Miocene to Recent tectonic history of the Capo Granitola and Sciacca fault systems offshore southwestern Sicily. These two fault arrays are part of a regional system of transcurrent faults t…

Fold growth rate010504 meteorology & atmospheric sciencesLate Miocene010502 geochemistry & geophysicsNeogene01 natural sciencesTranspressionMultiscale analysiSW Sicily offshorePaleontologyStrike-slip faultBasin inversion; Fold growth rates; Multiscale analysis; Pelagian foreland; Strike-slip faults; SW Sicily offshoreBasin inversionForeland basin0105 earth and related environmental sciencesEarth-Surface Processesgeographygeography.geographical_feature_categoryAnticlineFold (geology)TectonicsGeophysicsFold and thrust beltPelagian forelandStrike-slip faultsFold growth ratesMultiscale analysisGeologyTectonophysics
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