Search results for " flat‐topped seamount"

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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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