Search results for "Petrology"

showing 10 items of 1516 documents

A revision of the structure and stratigraphy of pre-Green Tuff ignimbrites at Pantelleria (Strait of Sicily)

2013

International audience; At Pantelleria, peralkaline silicic magmas were erupted across a range of eruptive typologies and magnitudes: pyroclastic flows, Plinian to strombolian pumice fallout and lava flows. In this paper we focus on the intermediate cycle of eruptive activity which is bracketed by ignimbrite units slightly older than the two caldera collapses which marked the volcanological activity of the island. This age interval (180-85 ka) was punctuated by six ignimbrite-forming eruptions (silicic and variably peralkaline) for a cumulative erupted magma volume of approximately 6 km3 dense rock equivalent. Based on new 40Ar/39Ar (Na,K)-feldspar ages and petrographic data, we propose an …

pantellerite010504 meteorology & atmospheric sciencesLava[SDE.MCG]Environmental Sciences/Global ChangesGeochemistrySilicicPyroclastic rock010502 geochemistry & geophysics01 natural sciencesPeralkaline rock40Ar/39Ar datingGeochemistry and PetrologyPumiceperalkaline magma[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyCalderaPeralkaline magmasGeomorphology0105 earth and related environmental sciencesIgnimbritesSettore GEO/07 - Petrologia E PetrografiaStrombolian eruptionignimbriteGeophysicsDense-rock equivalentPantellerites40Ar/39Ar dating.GeologyPantelleria
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Crystal field and magnetism with Wannier functions: Rare-earth doped aluminum garnets

2015

Using the recently developed method we calculate the crystal field parameters in yttrium and lutetium aluminum garnets doped with seven trivalent Kramers rare-earth ions. We then insert calculated parameters into the atomic-like Hamiltonian taking into account the electron-electron, spin-orbit and Zeeman interactions and determine the multiplet splitting by the crystal field as well as magnetic $\hat{g}$ tensors. We compare calculated results with available experimental data.

rare earthsWannier functionZeeman effectStrongly Correlated Electrons (cond-mat.str-el)Condensed matter physicsMagnetismab initio calculationsFOS: Physical scienceschemistry.chemical_elementGeneral ChemistryYttriumLutetiumIongarnetssymbols.namesakeCondensed Matter::Materials ScienceCondensed Matter - Strongly Correlated ElectronschemistryGeochemistry and PetrologysymbolsCondensed Matter::Strongly Correlated ElectronsHamiltonian (quantum mechanics)crystal fieldMultiplet
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The crater lake of Ilamatepec (Santa Ana) volcano, El Salvador: insights into lake gas composition and implications for monitoring

2019

We here present the first chemical characterization of the volcanic gas plume issuing from the Santa Ana crater lake, a hyper-acidic crater lake (pH of − 0.2 to 2.5) in north-western El Salvador. Our results, obtained during regular surveys in 2017 and 2018 using a Multi-GAS instrument, demonstrate a hydrous gas composition (H2O/SO2 ratios from 32 to 205) and SO2 as the main sulfur species (H2S/SO2 = 0.03–0.1). We also find that gas composition evolved during our investigated period, with the CO2/SO2 ratio decreasing by one order of magnitude from March 2017 (37.2 ± 9.7) to November 2018 (< 3). This compositional evolution toward more magmatic (SO2-rich) compositions is interpreted in the c…

ratio010504 meteorology & atmospheric sciences/SOGeochemistry2FluxContext (language use)010502 geochemistry & geophysics01 natural sciencesVolcanic gas plumeGeochemistry and PetrologyCrater lakeWet volcanoGas compositionPrecipitation0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryPlumeSanta Ana volcanoCOVolcanoVolume (thermodynamics)Crater lakeGas scrubbingGeologyMulti-GAS
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A method for measuring wetting and swelling of bentonite using X-ray imaging

2022

A non-invasive method based on X-ray imaging for measuring deformation and water transport in wetting and swelling bentonite samples is introduced. Sequential X-ray images taken of the samples were used to calculate the attenuation coefficient and deformation. These results, together with careful calibration, allowed finding the dry density and water content distributions and their temporal evolution in the wetting and swelling samples. A specific correction technique, based on regularly taking reference X-ray images of aluminum plates of varying thickness, was developed and used to take into account X-ray beam instabilities and thus to improve the accuracy of density analysis. Large deform…

röntgenkuvausGeochemistry and PetrologytomografiaX-ray imagingbentoniittivesiGeologySwellingvesipitoisuussavikulkeutuminenDeformation
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Stress sensitivity of stylolite morphology

2009

International audience; Stylolites are rough surfaces that form by localized stress-induced dissolution. Using a set of limestone rock samples collected at different depths from a vertical section in Cirque de Navacelles (France), we study the influence of the lithostatic stress on the stylolites morphology on the basis of a recent morphogenesis model. We measured the roughness of a series of bedding-parallel stylolites and show that their morphology exhibits a scaling invariance with two self-affine scaling regimes separated by a crossover-length (L) at the millimeter scale consistent with previous studies. The importance of the present contribution is to estimate the stylolite formation s…

self-affine scalingMorphology (linguistics)010504 meteorology & atmospheric sciences[SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]MineralogyMagnitude (mathematics)morphogenesisSurface finish010502 geochemistry & geophysics01 natural sciencesStress (mechanics)Geochemistry and Petrology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryEarth and Planetary Sciences (miscellaneous)Geotechnical engineeringpaleo-stressScaling0105 earth and related environmental sciencesroughness[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/TectonicsDeformation (mechanics)stylolitesStress fieldGeophysicsSpace and Planetary ScienceStyloliteGeology[SDU.STU.MI]Sciences of the Universe [physics]/Earth Sciences/Mineralogy
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In situ measurements of background aerosol and subvisible cirrus in the tropical tropopause region

2002

[1] In situ aerosol measurements were performed in the Indian Ocean Intertropical Convergence Zone (ITCZ) region during the Airborne Polar Experiment-Third European Stratospheric Experiment on Ozone (APE-THESEO) field campaign based in Mahe, Seychelles between 24 February and 6 March 1999. These are measurements of particle size distributions with a laser optical particle counter of the Forward Scattering Spectrometer Probe (FSSP)-300 type operated on the Russian M-55 high-altitude research aircraft Geophysica in the tropical upper troposphere and lower stratosphere up to altitudes of 21 km. On 24 and 27 February 1999, ultrathin layers of cirrus clouds were penetrated by Geophysica directly…

subvisualAtmospheric ScienceParticle numberMeteorologyaerosolsubvisible cirrusSoil SciencecirrusAquatic ScienceOceanographyAtmospheric sciencestropicsTroposphereGeochemistry and Petrologytropopauseddc:550Earth and Planetary Sciences (miscellaneous)StratosphereEarth-Surface ProcessesWater Science and TechnologyEcologybackgroundPaleontologyForestryJAerosolGeophysicsLidarSpace and Planetary ScienceEnvironmental scienceCirrusTropopauseParticle counterJournal of Geophysical Research: Atmospheres
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Phase equilibria of Pantelleria trachytes (Italy): constraints on pre-eruptive conditions and on the metaluminous to peralkaline transition in silici…

2018

Pantelleria Island is the type locality of pantellerite, an iron and alkali-rich rhyolite (P.I=molar Na2O+K2O/Al2O3 &gt;1.05). Peralkaline rhyolites (i.e pantellerite and comendite) and trachytes usually represent the felsic end-members in continental rift systems (e.g., Pantelleria, Tibesti, Ethiopia, Afar, Kenya, Bain and Range, South Greenland) and in oceanic sland settings (Socorro Is., Easter Is., Iceland and Azores). The origin of peralkaline rhyolites in the different tectonic settings is still a matter of debate and three hypotheses have been suggested: (a) crystal fractionation of alkali-basalt in a shallow reservoir to produce a trachyte which subsequently gives rise to a pantelle…

trachytepantellerite010504 meteorology & atmospheric sciencesliquid line of descentAnalytical chemistry[SDU.STU]Sciences of the Universe [physics]/Earth SciencesLiquidusengineering.materialmetaluminous–peralkaline transition010502 geochemistry & geophysics01 natural sciencesPeralkaline rocklaw.inventionGeochemistry and Petrologylawexperimental petrology[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/Volcanology62 pantelleriteCrystallizationperalkaline silicic magmatism0105 earth and related environmental sciencesBasaltFelsicFractional crystallization (geology)OlivineSettore GEO/07 - Petrologia E PetrografiaGeophysics[SDU]Sciences of the Universe [physics]13. Climate action63 liquid line of descentmetaluminous-peralkaline transitionengineeringAlkali feldsparGeologyPantelleria
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Experimental Constraints on the Deep Magma Feeding System at StromboliVolcano, Italy

2009

International audience; New experiments have been performed on a high-K basalt (PST-9) from Stromboli volcano, Italy, to constrain the physical conditions of golden pumice magmas at their storage level and discuss their petrogenesis. Fluid-present, H2O- and CO2-bearing, near-liquidus experiments were performed at 11508C between 100 and 400MPa and under oxidizing conditions. Glasses were analyzed by Fourier transform IR spectroscopy and their H2O and CO2 concentrations compared with those in glass inclusions.Most glass inclusions cluster near the 200MPa isobar, suggesting entrapment at a depth of ~8 km. Golden pumice magmas have viscosities of 7.9 Pa s and densities of 2.48-2.57 g/cm3. Compo…

ultra-calcic melts010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global ChangesMineralogyLiquidus010502 geochemistry & geophysics01 natural sciencesphysical propertiesGeochemistry and PetrologyPumiceexperimental petrology[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyStromboli0105 earth and related environmental sciencesMelt inclusionsPetrogenesisBasaltgeographygeography.geographical_feature_categorygolden pumiceSettore GEO/07 - Petrologia E PetrografiaGeophysicsVolcano13. Climate actionMagmaexperimental petrology Stromboli yellow pumicePrimitive mantlemagma storageGeology
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Ultra-high temperature metamorphism recorded in Fe-rich olivine-bearing migmatite from the Khondalite Belt, North China Craton

2018

International audience; We document the first occurrence of Fe‐rich olivine‐bearing migmatitic metapelite in the Khondalite Belt, North China Craton. Petrological analyses revealed two exotic assemblages of orthopyroxene+spinel+olivine and orthopyroxene+spinel+cordierite. Phase relation modelling suggests that these assemblages are diagnostic of ultra‐high temperature (UHT) metamorphism in the Fe‐rich system, with temperatures from 1,000 to 1,050°C at 0.6 GPa. U–Th–Pb SIMS analyses on zircon reveal a similar age of c. 1.92 Ga for the olivine‐bearing migmatite and an adjacent gabbronoritic intrusion that is therefore identified as the heat source for the UHT metamorphism. These results, coup…

ultra-high temperature metamorphism010504 meteorology & atmospheric sciencesGeochemistry[SDU.STU.PE]Sciences of the Universe [physics]/Earth Sciences/PetrographyMetamorphismengineering.material010502 geochemistry & geophysics01 natural sciencesNorth China CratonKhondalite BeltGeochemistry and PetrologymigmatitesPetrology0105 earth and related environmental sciences[ SDU.STU.PE ] Sciences of the Universe [physics]/Earth Sciences/Petrographygeographygeography.geographical_feature_categoryOlivineUltra-high-temperature metamorphismGeologymetamorphic olivineMigmatiteGranuliteCraton13. Climate actionengineeringKhondaliteMaficGeology
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Alteration-Induced Volcano Instability at La Soufrière de Guadeloupe (Eastern Caribbean)

2021

International audience; Volcanoes are unstable structures that deform laterally and frequently experience mass wasting events. Hydrothermal alteration is often invoked as a mechanism that contributes significantly to volcano instability. We present a study that combines laboratory experiments, geophysical data, and large-scale numerical modeling to better understand the influence of alteration on volcano stability, using La Soufrière de Guadeloupe (Eastern Caribbean) as a case study. Laboratory experiments on variably altered (advanced argillic alteration) blocks show that uniaxial compressive strength, Young's modulus, and cohesion decrease as a function of increasing alteration, but that …

upscalingVolcanic hazards010504 meteorology & atmospheric sciencesYoung's modulusMass wasting010502 geochemistry & geophysics01 natural sciencesInstabilityHydrothermal circulationGeochemistry and PetrologyFriction angleEarth and Planetary Sciences (miscellaneous)Cohesion (geology)[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyArgillic alterationPetrologyhydrothermal alterationuniaxial compressive strength0105 earth and related environmental sciencesflank collapsegeographygeography.geographical_feature_categoryGeophysicsVolcano13. Climate actionSpace and Planetary ScienceGeology
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