Search results for "Mantle flow"

showing 2 items of 2 documents

Present-day uplift of the European Alps: Evaluating mechanisms and models of their relative contributions

2019

Abstract Recent measurements of surface vertical displacements of the European Alps show a correlation between vertical velocities and topographic features, with widespread uplift at rates of up to ~2–2.5 mm/a in the North-Western and Central Alps, and ~1 mm/a across a continuous region from the Eastern to the South-Western Alps. Such a rock uplift rate pattern is at odds with the horizontal velocity field, characterized by shortening and crustal thickening in the Eastern Alps and very limited deformation in the Central and Western Alps. Proposed mechanisms of rock uplift rate include isostatic response to the last deglaciation, long-term erosion, detachment of the Western Alpine slab, as w…

European Alps Vertical displacement rate Deglaciation Erosion Lithospheric structural changes Mantle flowVertical displacement rate010504 meteorology & atmospheric sciencesEuropean AlpPresent day010502 geochemistry & geophysics01 natural sciencesPaleontologyLithospheric structural changesMantle convectionLithosphereDeglaciationddc:550ComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciences[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/TectonicsDeglaciationMantle flow15. Life on landLithospheric structural changeTectonics13. Climate actionErosionSlabGeneral Earth and Planetary SciencesUpwellingEuropean AlpsEarth and Planetary Sciences (all)Surface massGeology
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Magmatism Along Lateral Slab Edges: Insights From the Diamante-Enotrio-Ovidio Volcanic-Intrusive Complex (Southern Tyrrhenian Sea)

2019

Volcanic‐intrusive complexes often formed along lateral slab edges as a consequence of subduction‐induced mantle flow. We investigate this process in the southern Tyrrhenian Sea by integrating multibeam bathymetry, seismic‐reflection data, regional magnetic anomalies data, and seismological data. The interpretation of the data highlights the presence of magmatic intrusions that locally reach the seafloor forming volcanic edifices. Chimneys, lava flows, and laccoliths are observed beneath and surrounding the volcanoes. The emplacement and cooling of the magma occurred during the Brunhes Chron. The volcanoes are not active even if the hydrothermal activity occurs. The volcanic‐intrusive compl…

Tyrrhenian Seageographygeography.geographical_feature_categorySettore GEO/02 - Geologia Stratigrafica E Sedimentologicacalabrian acrccalabrian acrc; flat-topped seamount; slab tearing; STEP fault; subduction-induced mantle flow; Tyrrhenian SeaSettore GEO/03 - Geologia StrutturaleGeochemistryflat-topped seamountsubduction-induced mantle flowCalabrian Arc; flat-topped seamount; slab tearing; STEP fault; subduction-induced mantle flow; Tyrrhenian SeaCalabrian ArcGeophysicsCalabrian Arc Tyrrhenian Sea Subduction-induced mantle flow STEP fault slab tearing flat-topped seamount.VolcanoGeochemistry and PetrologySettore GEO/11 - Geofisica ApplicataMagmatismSlabslab tearingGeologySTEP faultCalabrian Arc Tyrrhenian Sea subduction induced mantle flow STEP fault slab tearing flat‐topped seamount
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