Search results for "pumice"

showing 10 items of 35 documents

Submarine deposits from pumiceous pyroclastic density currents traveling over water: An outstanding example from offshore Montserrat (IODP 340)

2017

© 2016. Geological Society of America. All right reserved. Pyroclastic density currents have been observed to both enter the sea, and to travel over water for tens of kilometers. Here, we identified a 1.2-m-thick, stratified pumice lapilli-ash cored at Site U1396 offshore Montserrat (Integrated Ocean Drilling Program [IODP] Expedition 340) as being the first deposit to provide evidence that it was formed by submarine deposition from pumice-rich pyroclastic density currents that traveled above the water surface. The age of the submarine deposit is ca. 4 Ma, and its magma source is similar to those for much younger Soufrière Hills deposits, indicating that the island experienced large-magnitu…

Turbidity currentExplosive eruption010504 meteorology & atmospheric sciencesGeochemistryPyroclastic rockGeology010502 geochemistry & geophysics01 natural sciencesSubmarine eruptionGeophysicsGeochemistryPyroclastic surgePumiceSubaerial[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/Volcanology14. Life underwaterPyroclastic fallLife Below WaterGeomorphologyGeology0105 earth and related environmental sciencesGeological Society of America Bulletin
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The pumice aggregates of Lipari Island (Aeolian Isles-Italy)

1984

In the Island of Lipari (Aeolian Archipelago) there is a large pumice deposit. The pumice is exploited in an open-cast mine through mechanical means and taken to crushing and screening plants. Aggregates for urban construction, gravel and powder are obtained. The aggregates are used in the manufacture of light concrete. Nowadays the possibility of using pumice aggregates in order to obtain light structural concrete is being studied.

Nature ConservationPumiceGeochemistryAeolian processesGeologyGeotechnical Engineering and Engineering GeologyGeomorphologyUrban constructionGeologyAeolian archipelagoBulletin of the International Association of Engineering Geology
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Volatile dilution during magma injections and implications for volcano explosivity

2016

Magma reservoirs underneath volcanoes grow through episodic emplacement of magma batches. These pulsed magma injections can substantially alter the physical state of the resident magma by changing its temperature, pressure, composition, and volatile content. Here we examine plagioclase phenocrysts in pumice from the 2014 Plinian eruption of Kelud (Indonesia) that record the progressive capture of small melt inclusions within concentric growth zones during crystallization inside a magma reservoir. High-spatial-resolution Raman spectroscopic measurements reveal the concentration of dissolved H2O within the melt inclusions, and provide insights into melt-volatile behavior at the single crystal…

Dewey Decimal Classification::500 | Naturwissenschaften::550 | GeowissenschaftenAsiaFar East010504 meteorology & atmospheric sciencesinclusionspyroclasticsMineralogyVolcanic explosivity indexengineering.material010502 geochemistry & geophysicsAnorthite01 natural sciencespumicePumiceddc:550PlagioclaseFluid inclusionsPetrology0105 earth and related environmental sciencesMelt inclusionsGeologyGeokemimagmasGeochemistryfluid inclusionsIndonesiaigneous rocksMagmaengineeringPhenocrystvolcanic rocksJavaGeology
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Volatiles in pantellerite magmas: A case study of the Green Tuff Plinian eruption (Island of Pantelleria, Italy)

2013

Abstract The Green Tuff (GT) Plinian eruption, the largest in magnitude at Pantelleria, erupted 3 to 7 km3 DRE of pantellerite magma and a small volume of trachyte. Fifty-nine anorthoclase-hosted melt inclusions from the two basal pumice members were analyzed by FT-IR spectroscopy in order to assess the pre-eruptive H2O content in the pantellerite melt. Microanalytical methods were used to determine major element, Cl, F and S contents. Melt inclusions and glassy groundmasses have a nearly homogeneous pantelleritic composition (peralkaline index = 1.9-2.2) and variable water contents ranging from 1.4 to as high as 4.2 wt %, i.e. much higher than the 1.4 wt % of earlier published studies. The…

LavaSettore GEO/07 - Petrologia E PetrografiaGeochemistryTrachyteMagma chamberStrombolian eruptionGeophysicsEffusive eruptionGeochemistry and PetrologyPumiceMagmaThe Green Tuff (GT) Plinian eruption the largest in magnitude at Pantelleria erupted 3 to 7 km 3 DRE of pantellerite magma and a small volume of trachyte. Fifty-nine anorthoclase-hosted melt inclusions from the two basal pumice members were analyzed by FT-IR spectroscopy in order to assess the pre-eruptive H2Ocontent in the pantellerite melt. Microanalytical methods were used to determine major element Cl F and S contents. Melt inclusions and glassy groundmasses have a nearly homogeneous pantelleritic composition (peralkaline index = 1.9-2.2) and variable water contents ranging from 1.4 to as high as 4.2 wt % i.e. much higher than the 1.4 wt % of earlier published studies. The chlorine content is constant at about 1 wt %. Combined Cl and H2O data were used to estimate a confining pressure of about 50 MPa (depth around 2-3 km) for the GT magma chamber. The chamber was characterized by a compositional zoning with a dominant pantellerite overlying a trachyte magma. Soon after the GT eruption intra-caldera volcanism was dominated by the eruption of voluminous trachyte lavaflows while pantellerite melt production resumed after about 20 ka with numerous low-volume mildly explosive (Strombolian) to effusive eruptions. Comparison with data from the literature reveals that despite the differentexplosivity the post-caldera Strombolian eruptions and the GT Plinian eruption were fed by pantelleritic magmas with similar water contents. Chlorine and CO2contents suggest that the young magma reservoirs feeding the Strombolian to effusive activity were deeper (h≥4.5 km) than the much larger (based on erupted volumes) magma chamber which fed the GT eruptionGeologyMelt inclusionsJournal of Volcanology and Geothermal Research
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Outgassing: Influence on speed of magma fragmentation

2013

[1] Predicting explosive eruptions remains an outstanding challenge. Knowledge of the controlling parameters and their relative importance is crucial to deepen our understanding of conduit flow dynamics and accurately model the processes involved. This experimental study sheds light on one important parameter—outgassing—and evaluates its influence on magma fragmentation behavior. We perform fragmentation experiments based on the shock tube theory at room temperature on natural pyroclastic material with a connected porosity ranging from 15% to 78%. For each sample series, we determine the initial pressure (P) required to initiate magma fragmentation (fragmentation threshold, Pth). Furthermor…

Explosive eruption010504 meteorology & atmospheric sciencesPyroclastic rock010502 geochemistry & geophysics01 natural sciencesOutgassingGeophysicsElectrical conduitFragmentation (mass spectrometry)13. Climate actionSpace and Planetary ScienceGeochemistry and PetrologyPumiceEarth and Planetary Sciences (miscellaneous)Geotechnical engineeringScoriaShock tubePetrologyGeology0105 earth and related environmental sciencesJournal of Geophysical Research: Solid Earth
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The use and beauty of ultra-high-resolution seismic reflection imaging in Late Quaternary marine volcaniclastic settings, Napoli Bay, Italy

2019

A Nápolyi-öbölben felvett ultra nagy felbontású egycsatornás (IKB-Seistec™) reflexiós szeizmikus szelvények korábbi geológiai és geofizikai vizsgálatok eredményeivel együtt kivételes, eddig soha nem látott felbontású szeizmikus leképezését nyújtják a Flegrei-mezők és a Somma-Vezúv felszín alá süllyedt késő-pleisztocén–holocén rétegtani felépí - tésének. A szeizmikus szelvényeken látott geometria és gravitációs magvevővel nyert üledékek adatainak összevetéséből Campania partközeli kontinentális talapzatán számos olyan üledékes és vulkáni szerkezet, valamint hidrotermális jelenség került leképezésre, melyek a legutolsó glaciális maximum (kb. 18 000 év) óta keletkeztek. A Pozzuoli-öbölben mért…

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/03 - Geologia StrutturaleStratigraphyVolcaniclastic settingsPyroclastic rockFault (geology)PaleontologyGeochemistry and PetrologyPumiceCampania VolcanismStratovolcanoSomma-Vesuviushigh-resolution single channel reflection seismics Campania Volcanism Volcaniclastic settings Campi Flegrei Caldera ring fault Somma-Vesuvius Late Quaternary Bay of Naplesgeographygeography.geographical_feature_categoryContinental shelfResurgent domePaleontologyCaldera ring faultGeologyLate QuaternarySeafloor spreadingVolcanoHigh-resolution single channel reflection seismicsBay of NaplesCampi FlegreiGeologyFöldtani Közlöny
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The structure of pumice: An XPS and27Al MAS NMR study

1992

In order to investigate the surface structure of pumice, an amorphous aluminosilicate, samples of pumice and of standards of silica and alumina have been studied by x-ray photoelectron spectroscopy (XPS). The effect of a mild acid leaching was also considered. The analysis of the Si 2p, Al 2p and O 1s photoelectron peaks and the Si KLL and O KLL Auger peaks indicated that pumice is formed by tetrahedral silica with some units being replaced by aluminate, AlO2−. The acid treatment decreases the alkali and the aluminate ions. X-ray photoelectron spectra of the valence band of pumices and of standards of Al2O3 and SiO2 agree with the core-level results. To support the conclusions from the XPS …

ChemistryAluminateAnalytical chemistrychemistry.chemical_elementSurfaces and InterfacesGeneral ChemistryCondensed Matter PhysicsAlkali metalSurfaces Coatings and FilmsAmorphous solidchemistry.chemical_compoundNuclear magnetic resonanceX-ray photoelectron spectroscopyAluminiumAluminosilicatePumiceMaterials ChemistryMagic angle spinningSurface and Interface Analysis
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EXAFS and XRD study of Pd–Ag bimetallic catalysts supported on pumice from organometallic precursors

2001

Abstract Silver–palladium bimetallic catalysts were supported on pumice following different procedures, based on mild treatments of organometallic precursors. The experiments for the structural characterization of the synthesized samples, wide angle X-ray diffraction (XRD) and X-ray absorption spectroscopy, were carried out at the beamline GILDA of the European Synchrotron Radiation Facility. The analysis of the data demonstrated that alloying took place with a degree of homogeneity depending on the different preparation routes.

Absorption spectroscopyExtended X-ray absorption fine structureChemistrychemistry.chemical_elementCondensed Matter PhysicsElectronic Optical and Magnetic MaterialsCatalysisCrystallographyTransition metalPumiceX-ray crystallographyMaterials ChemistryCeramics and CompositesBimetallic stripPalladiumNuclear chemistryJournal of Non-Crystalline Solids
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The holocene marine record of unrest, volcanism, and hydrothermal activity of campi flegrei and somma-vesuvius

2020

Abstract This chapter illustrates the marine record of a spectrum of volcanic, hydrothermal, and sedimentary features that characterize the Latest Pleistocene–Holocene evolution of the Naples Bay offshore Campi Flegrei and Somma–Vesuvius. The work is based on review of previous literature integrated with interpretation of new high-resolution marine Digital Terrain Models (DTMs) derived from swath bathymetry surveys and high-resolution reflection seismic profiles calibrated with marine gravity core data. Seismic profiles from Pozzuoli Bay provide detailed images of the ring fault system and resurgent dome associated with the evolution of the Neapolitan Yellow Tuff (NYT) collapse caldera and …

geographygeography.geographical_feature_categorySettore GEO/02 - Geologia Stratigrafica E SedimentologicaCampania volcanismResurgent domeSettore GEO/03 - Geologia StrutturaleGeochemistrySommavesuviusPyroclastic rockEastern tyrrhenian marginVolcanismFault (geology)Naples baySeafloor spreadingVolcanoPumiceCampi flegreiHolocene marine recordCalderaGeology
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Pumice concrete for structural wall panels

2003

Some properties of lightweight pumice stone concrete (LWPSC) are discussed, on account of a possible structural use of this material. Then the results of an experimental investigation are described, in order to show that pumice can really be considered an alternative to common artificial lightweight aggregates, taking into account the performance pointed out by loading tests carried out on structural systems made of LWPSC. Three different kinds of reinforced wall panels were made using LWPSC, lightweight expanded clay concrete and normal weight concrete; then their structural responses under horizontal cyclic and constant vertical forces were compared, above all with reference to lateral st…

Materials scienceAggregate (composite)business.industryStructural systemPumice aggregateStructural engineeringStructural lightweight concreteStructural elementSettore ICAR/09 - Tecnica Delle CostruzioniCrackingStructural loadPumiceShear wallGeotechnical engineeringSquat reinforced concrete wallbusinessMaterial propertiesCivil and Structural EngineeringEngineering Structures
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