Search results for "MAGMA"

showing 10 items of 262 documents

Phase petrology reveals shallow magma storage prior to large explosive silicic eruptions at Hekla volcano, Iceland

2017

Abstract Understanding the conditions that culminate in explosive eruptions of silicic magma is of great importance for volcanic hazard assessment and crisis mitigation. However, geological records of active volcanoes typically show a wide range of eruptive behavior and magnitude, which can vary dramatically for individual eruptive centers. In order to evaluate possible future scenarios of eruption precursors, magmatic system variables for different eruption types need to be constrained. Here we use petrological experiments and microanalysis of crystals to clarify the P – T – x state under which rhyodacitic melts accumulated prior to the H3 eruption; the largest Holocene Plinian eruption of…

geographyVulcanian eruptionExplosive eruptiongeography.geographical_feature_category010504 meteorology & atmospheric sciencesGeochemistrySilicicMagma chamber010502 geochemistry & geophysics01 natural sciencesGeophysicsVolcanoSpace and Planetary ScienceGeochemistry and PetrologyPumiceMagmaddc:550Earth and Planetary Sciences (miscellaneous)PhenocrystPetrologyGeology0105 earth and related environmental sciencesEarth and Planetary Science Letters
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Turmoil at Turrialba Volcano (Costa Rica): Degassing and eruptive processes inferred from high-frequency gas monitoring

2016

Eruptive activity at Turrialba Volcano (Costa Rica) has escalated significantly since 2014, causing airport and school closures in the capital city of San Jose. Whether or not new magma is involved in the current unrest seems probable but remains a matter of debate as ash deposits are dominated by hydrothermal material. Here we use high-frequency gas monitoring to track the behavior of the volcano between 2014 and 2015 and to decipher magmatic versus hydrothermal contributions to the eruptions. Pulses of deeply derived CO2-rich gas (CO2/S-total>4.5) precede explosive activity, providing a clear precursor to eruptive periods that occurs up to 2weeks before eruptions, which are accompanied by…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesEarth scienceGeochemistryGas emissions010502 geochemistry & geophysics01 natural sciencesHydrothermal circulationGas monitoringMagmatic waterGeophysicsVolcano13. Climate actionSpace and Planetary ScienceGeochemistry and PetrologyCapital cityEarth and Planetary Sciences (miscellaneous)Phreatomagmatic eruptionPhreaticGeology0105 earth and related environmental sciencesJournal of Geophysical Research: Solid Earth
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H2O-content and temperature limit the explosive potential of rhyolite magma during Plinian eruptions

2019

Abstract Recent rhyolite eruptions on Earth have demonstrated their capacity to produce a multitude of hazards, including ash formation lasting months and impacting the large reaches of the southern hemisphere. Nevertheless, the underlying mechanisms driving these eruptions are not yet fully understood. Magmatic volatiles, especially H2O, dictate whether volcanic eruptions proceed explosively or effusively. Experimental evidence for the role played by H2O in driving explosive fragmentation is rare, in particular in the eruption of rhyolitic magma. Here we show that when hydrous rhyolitic obsidians from Chaiten Volcano (Chile) are experimentally heated above their glass transition temperatur…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesExplosive materialFragmentation (computing)Pyroclastic rock010502 geochemistry & geophysics01 natural sciencesOverpressureGeophysicsVolcanoSpace and Planetary ScienceGeochemistry and PetrologyRhyoliteMagmaEarth and Planetary Sciences (miscellaneous)PetrologyGeologyPressure gradient0105 earth and related environmental sciencesEarth and Planetary Science Letters
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First observations of the fumarolic gas output from a restless caldera: Implications for the current period of unrest (2005-2013) at Campi Flegrei

2013

[1] The fumarolic gas output has not been quantified for any of the currently deforming calderas worldwide, due to the lack of suitable gas flux sensing techniques. In view of resumption of ground uplift (since 2005) and the associated variations in gas chemistry, Campi Flegrei, in southern Italy, is one of the restless calderas where gas flux observations are especially necessary. Here we report the first ever obtained estimate of the Campi Flegrei fumarolic gas output, based on a set of MultiGAS surveys (performed in 2012 and 2013) with an ad-hoc-designed measurement setup. We estimate that the current Campi Flegrei fumarolic sulphur (S) flux is low, on the order of 1.5–2.2 tons/day, sugg…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesFluxCurrent periodUnrest010502 geochemistry & geophysics01 natural sciencesHydrothermal circulationchemistry.chemical_compoundGeophysicsVolcanochemistry13. Climate actionGeochemistry and PetrologyCarbon dioxideMagmaCalderaPetrologyGeologySeismology0105 earth and related environmental sciencesGeochemistry, Geophysics, Geosystems
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Multi-component gas emission measurements of the active lava lake of Nyiragongo, DR Congo

2017

Between 2007 and 2011 four measurement campaigns (June 2007, July 2010, June 2011, and December 2011) were carried out at the crater rim of Nyiragongo volcano, DR Congo. Nyiragongo is one of the most active volcanoes in Africa. The ground-based remote sensing technique Multi-Axis Differential Optical Absorption Spectroscopy (MAX-DOAS), which uses scattered sunlight, the in-situ Multi-Component Gas Analyzer System (Multi-GAS) and alkaline impregnated filter were simultaneously applied during all field trips. The bromine monoxide to sulfur dioxide (BrO/SO2) and carbon dioxide to sulfur dioxide (CO2/SO2) molar ratios were determined, among other ratios. During the different field trips variati…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesLavaDifferential optical absorption spectroscopyMineralogyGeology010502 geochemistry & geophysics01 natural sciencesLava lake level changeGas analyzerPlumechemistry.chemical_compoundNyiragongochemistryVolcanoCarbon dioxideMagmaGas compositionGas composition variationGeology0105 earth and related environmental sciencesEarth-Surface Processes
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Insights into magma and fluid transfer at Mount Etna by a multiparametric approach: A model of the events leading to the 2011 eruptive cycle

2013

[1] Since the second half of the 1990s, the eruptive activity of Mount Etna has provided evidence that both explosive and effusive eruptions display periodic variations in discharge and eruption style. In this work, a multiparametric approach, consisting of comparing volcanological, geophysical, and geochemical data, was applied to explore the volcano's dynamics during 2009–2011. In particular, temporal and/or spatial variations of seismicity (volcano-tectonic earthquakes, volcanic tremor, and long-period and very long period events), ground deformation (GPS and tiltmeter data), and geochemistry (SO2 flux, CO2 flux, CO2/SO2 ratio) were studied to understand the volcanic activity, as well as…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesLavaInversion (geology)TiltmeterVolcanology010502 geochemistry & geophysics01 natural sciencesGeophysicsEffusive eruptionVolcanoImpact crater13. Climate actionSpace and Planetary ScienceGeochemistry and PetrologyMagmaEarth and Planetary Sciences (miscellaneous)SeismologyGeology0105 earth and related environmental sciencesJournal of Geophysical Research: Solid Earth
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The summit hydrothermal system of Stromboli: New insights from self-potential, temperature, CO2 and fumarolic fluids measurements, with structural an…

2003

International audience; Accurate and precisely located self-potential (SP), temperature (T) and COi measurements were carried out in the summit area of Stromboli along 72 straight profiles. SP data were acquired every metre and T data every 2.5 m. CO2 concentrations were acquired with the same density as T, but only along seven profiles. The high density of data and the diversity of the measured parameters allows us to study structures and phenomena at a scale rarely investigated. The shallow summit hydrothermal activity (Pizzo-Fossa area) is indicated by large positive SP, T and COi anomalies. These anomalies are focused on crater faults, suggesting that the fracture zones are more permeab…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesLava[SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]Soil gasMineralogyFault (geology)010502 geochemistry & geophysics01 natural sciencesFumaroleHydrothermal circulationImpact crater13. Climate actionGeochemistry and PetrologyPhreatomagmatic eruption[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyPetrologyGeologyPhreatic0105 earth and related environmental sciences
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Heterogeneity of volatile sources along the Halmahera arc, Indonesia

2021

co-auteur étranger; International audience; The parallel Halmahera and Sangihe arcs in eastern Indonesia are sites of active arc-arc collision of considerable interest in developing understanding of the geodynamics and geochemistry of subduction zones. Owing to the comparative remoteness of the region, few ground-based studies of the volcanoes have been undertaken. Here, we report and integrate gas measurements and (isotope) geochemical analyses of lava samples for Dukono, Ibu, Gamkonora, Gamalama, and Makian volcanoes of the Halmahera arc. Summing gas fluxes for all five volcanoes indicates arcscale emission budgets for H 2 O, CO 2 , SO 2 , H 2 S, and H 2 of 96300±27000, 2093±450, 944±400,…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesMantle wedgeSubductionLavaArc-scale degassing budget Halmahera volcanoes Sediment contribution and fluid flux Variability of arc magmaGeochemistryPartial meltingVariability of arc magmaCrustHalmahera volcanoesGeodynamics010502 geochemistry & geophysics01 natural sciencesMantle (geology)Sediment contribution and fluid fluxGeophysicsVolcano13. Climate actionGeochemistry and Petrology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyGeology0105 earth and related environmental sciences
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Extensive magmatism and metamorphism at ca. 3.2 Ga in the eastern Kaapvaal Craton

2020

Abstract The timing of the emergence of modern-style plate tectonics on Earth is of fundamental importance in understanding the thermal and compositional history of the planet. Although the magmatism and metamorphism in the eastern Kaapvaal Craton was thought by some as geological records for mid-Archean subduction at 3.2 Ga, their petrogenesis was fiercely debated. To reveal the nature of the 3.2 Ga magmatism and metamorphism in the eastern Kaapvaal Craton, here we provide a comprehensive zircon and monazite U-Pb geochronological investigation, coupled with in situ trace element and Hf-O isotopic analyses, for the magmatic and metamorphic rocks from the Barberton granitoid-greenstone terra…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesMetamorphic rockGeochemistryMetamorphismGeology010502 geochemistry & geophysicsGranulite01 natural sciencesCratonGeochemistry and PetrologyMagmatismGeologyMetamorphic facies0105 earth and related environmental sciencesZirconGneissPrecambrian Research
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Contribution of magmatism, partial melting buffering and localized crustal thinning on the late Variscan thermal structure of the Agly massif (French…

2020

International audience

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesThinningPartial meltingGeochemistryGeologyMassif010502 geochemistry & geophysics01 natural sciences[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryGeochemistry and PetrologyGeochronologyMagmatismComputingMilieux_MISCELLANEOUSGeology0105 earth and related environmental sciencesJournal of Metamorphic Geology
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