0000000000787255

AUTHOR

Ilenia Arienzo

showing 2 related works from this author

Degassing vs. eruptive styles at Mt. Etna volcano (Sicily, Italy). Part I: Volatile stocking, gas fluxing, and the shift from low-energy to highly ex…

2018

International audience; Basaltic magmas can transport and release large amounts of volatiles into the atmosphere, especially in subduction zones, where slab-derived fluids enrich the mantle wedge. Depending on magma volatile content, basaltic volcanoes thus display a wide spectrum of eruptive styles, from common Strombolian-type activity to Plinian events. Mt. Etna, in Sicily, is a typical basaltic volcano where the volatile control on such a variable activity can be investigated. Based on a melt inclusion study in products from Strombolian or lava-fountain activity to Plinian eruptions, here we show that for the same initial volatile content, different eruptive styles reflect variable dega…

Melt inclusion010504 meteorology & atmospheric sciencesExplosive materialMantle wedgeGeochemistryengineering.material010502 geochemistry & geophysics01 natural sciencesMicroliteGeochemistry and Petrology[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyBasaltic explosive volcanism0105 earth and related environmental sciencesMelt inclusionsBasaltgeographygeography.geographical_feature_categorySubductionMt. EtnaTotal volatilesChemical thermodynamicsGeologyTotal volatileStrombolian eruptionChemical thermodynamicVolcano13. Climate actionengineeringMelt inclusionsGeology
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Noble-gas signature of magmas from a heterogeneous mantle wedge: The case of Stromboli volcano (Aeolian Islands, Italy)

2014

Abstract We report on the variation of the elemental (He, Ne, and Ar) and isotopic (He and Ar) compositions of olivine- and clinopyroxene-hosted fluid inclusions hosted in lavas, pyroclastics, and cumulate xenoliths from the last 60 ka of the eruptive history of Stromboli volcano, Italy. Samples belong to (i) the present-day activity as represented by shoshonitic (SHO) basalts, i.e., pumices with low porphyritic (LP) content and high porphyritic (HP) scoriae; (ii) the subalkaline versus alkaline products erupted at Stromboli during its subaerial history among the extreme magmatic series, i.e., calc-alkaline (CA) and potassic (KS); and (iii) the only known ultramafic cumulates (San Bartolo w…

BasaltOlivineMantle wedgeGeochemistryGeologyengineering.materialFluid inclusionUltramafic cumulatesPorphyritic3He/4He ratioIgneous rockGeochemistry and PetrologyUltramafic rockengineeringSr-Nd isotopeXenolithStromboliMantleMaficGeologyChemical Geology
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