Search results for "Peralkaline volcanism"

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Volcanological evolution of Pantelleria Island (Strait of Sicily) peralkaline volcano: a review

2022

International audience; Pantelleria volcano has a particularly intriguing evolutionary history intimately related to the peralkaline composition of its explosively erupted magmas. Due to the stratigraphic complexity, studies over the last two decades have explored either only the pre-Green Tuff ignimbrite volcanism or the post-Green Tuff activity. We here focus on the whole evolutionary history, detailing the achievements since the first pioneering studies, in order to illustrate how the adoption and integration of progressively more accurate methods (40 Ar/ 39 Ar, paleomagnetism, petrography, and detailed field study) have provided many important independent answers to unresolved questions…

PaleomagnetismPaleomagnetism010504 meteorology & atmospheric sciences[SDU.STU]Sciences of the Universe [physics]/Earth SciencesVolcanismVolcanic explosivity index010502 geochemistry & geophysics01 natural sciencesPeralkaline rockPetrographyPaleontologyCalderaRheomorphism0105 earth and related environmental sciencesGeneral Environmental Sciencegeographygeography.geographical_feature_categoryIgnimbritesPeralkaline volcanismSettore GEO/07 - Petrologia E Petrografia40 Ar/ 39 ArVolcano[SDU]Sciences of the Universe [physics]Period (geology)General Earth and Planetary SciencesPeralkaline volcanism Ignimbrites Paleomagnetism 40Ar/39Ar RheomorphismGeology
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Explosive eruptive history of Pantelleria, Italy: Repeated caldera collapse and ignimbrite emplacement at a peralkaline volcano

2018

A new, pre-Green Tuff (46 ka) volcanic stratigraphy is presented for the peralkaline Pantelleria Volcano, Italy. New 40Ar/39Ar and paleomagnetic data are combined with detailed field studies to develop a comprehensive stratigraphic reconstruction of the island.We find that the pre-46 ka succession is characterised by eight silicarich peralkaline (trachyte to pantellerite) ignimbrites,many ofwhich blanketed the entire island. The ignimbrites are typically welded to rheomorphic, and are commonly associated with lithic breccias and/or pumice deposits. They record sustained radial pyroclastic density currents fed by lowpyroclastic fountains. The onset of ignimbrite emplacement is typically prec…

010504 meteorology & atmospheric sciencesGeochemistryPyroclastic rockTrachyte010502 geochemistry & geophysics01 natural sciencesPeralkaline rock40Ar/39Ar datingEffusive eruptionGeochemistry and PetrologyPumiceBreccia[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyCalderaEruptive history0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryIgnimbritesPeralkaline volcanismSettore GEO/07 - Petrologia E PetrografiaSettore GEO/08 - Geochimica E VulcanologiaCaldera collapsePeralkaline volcanism Pantelleria Ignimbrites Caldera collapse Eruptive history 40Ar/39Ar datingGeophysicsVolcano13. Climate actionSeismologyGeologyPantelleria
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