Search results for "Geophysics"

showing 10 items of 2645 documents

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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SST Comparison of AVHRR and MODIS Time Series in the Western Mediterranean Sea

2020

La temperatura de la superficie del mar (SST) es un parámetro clave para comprender los procesos atmosféricos y oceánicos. Desde finales de la década de 1980, las imágenes de satélite infrarrojas se han utilizado para complementar los registros in situ para estudiar la variabilidad temporal y espacial de la SST. El radiómetro avanzado de muy alta resolución (AVHRR) del satélite de la Administración Nacional Oceánica y Atmosférica (NOAA) fue el primer sensor utilizado con éxito para calcular la SST después del desarrollo y validación del algoritmo de corrección atmosférica conocido como 'ventana dividida'. Más recientemente, el espectrorradiómetro de imágenes de resolución MODERADA (MODIS) a…

validationMediterranean climate010504 meteorology & atmospheric sciencesAdvanced very-high-resolution radiometerAtmospheric correction010502 geochemistry & geophysics01 natural sciencesMarSea surface temperatureSpectroradiometerMediterranean seaMODISsea surface temperatureClimatologyMediterranean SeaGeneral Earth and Planetary SciencesEnvironmental sciencelcsh:QSatelliteSpatial variabilityAVHRR-NOAAmonitoring and error characterization of SSTlcsh:Science0105 earth and related environmental sciencesRemote Sensing
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A Low-Cost Smartphone Sensor-Based UV Camera for Volcanic SO2 Emission Measurements

2017

Recently, we reported on the development of low-cost ultraviolet (UV) cameras, based on the modification of sensors designed for the smartphone market. These units are built around modified Raspberry Pi cameras (PiCams; ≈USD 25), and usable system sensitivity was demonstrated in the UVA and UVB spectral regions, of relevance to a number of application areas. Here, we report on the first deployment of PiCam devices in one such field: UV remote sensing of sulphur dioxide emissions from volcanoes; such data provide important insights into magmatic processes and are applied in hazard assessments. In particular, we report on field trials on Mt. Etna, where the utility of these devices in quantif…

volcanic gas emissionsgeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesvolcano monitoringRaspberry Pilow-cost ultraviolet camera010502 geochemistry & geophysicsUSable01 natural sciences7. Clean energyRaspberry piVolcanoApplication areassulphur dioxideGeneral Earth and Planetary SciencesEnvironmental sciencelcsh:QSO<sub>2</sub> camera; Raspberry Pi; low-cost ultraviolet camera; volcanic gas emissions; sulphur dioxide; volcano monitoringlcsh:ScienceSO2 camera0105 earth and related environmental sciencesRemote sensingRemote Sensing
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A model of degassing for Stromboli volcano

2010

International audience; A better understanding of degassing processes at open-vent basaltic volcanoes requires collection of new datasets of H2O–CO2–SO2 volcanic gas plume compositions, which acquisition has long been hampered by technical limitations. Here, we use the MultiGAS technique to provide the best-documented record of gas plume discharges from Stromboli volcano to date. We show that Stromboli's gases are dominated by H2O (48–98 mol%; mean, 80%), and by CO2 (2–50 mol%; mean, 17%) and SO2 (0.2–14 mol%; mean, 3%). The significant temporal variability in our dataset reflects the dynamic nature of degassing process during Strombolian activity; which we explore by interpreting our gas m…

volcanic gase010504 meteorology & atmospheric sciencesEarth science010502 geochemistry & geophysics01 natural sciencesVolcanic Gasesvolcanic degassing; Stromboli; volcanic gases; CO2 fluxingGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)eventStromboliPetrology0105 earth and related environmental sciencesBasaltevent.disaster_typegeographygeography.geographical_feature_categoryStrombolian eruptionSettore GEO/08 - Geochimica E VulcanologiaPlumeGeophysicsVolcanovolcanic gases13. Climate actionSpace and Planetary ScienceMagmaCO2 fluxingInclusion (mineral)[SDU.OTHER]Sciences of the Universe [physics]/OtherSaturation (chemistry)volcanic degassingGeologyEarth and Planetary Science Letters
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Sulfur Degassing From Steam-Heated Crater Lakes: El Chichón (Chiapas, Mexico) and Víti (Iceland)

2018

The composition of the gases released by El Chichón (Chiapas, Mexico) and Víti (Askja volcano, Iceland) volcanic lakes is examined by Multi-GAS for the first time. Our results demonstrate that H2S and SO2 are degassed by these pH 2–3 lakes. We find higher CO2/H2S and H2/H2S ratios in the lakes' emissions (31–5,685 and 0.6–35, respectively) than in the fumarolic gases feeding the lakes (13–33 and 0.08–0.5, respectively), evidencing that only a fraction (0.2–5.4% at El Chichón) of the H2S(g) contributed by the subaquatic fumaroles ultimately reaches the atmosphere. At El Chichón, we estimate a H2S output from the crater lake of 0.02–0.06 t/day. Curiously, SO2 is also detected at trace levels …

volcanic lake010504 meteorology & atmospheric sciencesGeochemistrychemistry.chemical_elementVíti010502 geochemistry & geophysicssulfur degassing01 natural sciencesSulfurEl ChichónGeophysicsImpact craterchemistryGeneral Earth and Planetary SciencesGeophysicEarth and Planetary Sciences (all)Multi-GASGeology0105 earth and related environmental sciencesGeophysical Research Letters
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Volcanic Plume CO2 Flux Measurements at Mount Etna by Mobile Differential Absorption Lidar

2017

Volcanic eruptions are often preceded by precursory increases in the volcanic carbon dioxide (CO2) flux. Unfortunately, the traditional techniques used to measure volcanic CO2 require near-vent, in situ plume measurements that are potentially hazardous for operators and expose instruments to extreme conditions. To overcome these limitations, the project BRIDGE (BRIDging the gap between Gas Emissions and geophysical observations at active volcanoes) received funding from the European Research Council, with the objective to develop a new generation of volcanic gas sensing instruments, including a novel DIAL-Lidar (Differential Absorption Light Detection and Ranging) for remote (e.g., distal) …

volcanic plumes010504 meteorology & atmospheric sciencesFlux010502 geochemistry & geophysicsAtmospheric sciences01 natural sciencesVolcanic plumeVolcanic CO2 fluxImpact craterDifferential Absorption Lidar (DIAL);Remote sensing;Volcanic CO2 flux;Volcanic plumesGas compositionDifferential Absorption Lidar (DIAL)0105 earth and related environmental sciencesRemote sensinggeographygeography.geographical_feature_categoryvolcanic plumes; volcanic CO<sub>2</sub> flux; remote sensing; Differential Absorption Lidar (DIAL)lcsh:QE1-996.5ElevationRemote sensingPlumelcsh:GeologyLidarVolcanoVolcanic plume13. Climate actionGeneral Earth and Planetary SciencesEarth and Planetary Sciences (all)GeologyGeosciences; Volume 7; Issue 1; Pages: 9
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Ultraviolet imaging of volcanic plumes: A new paradigm in volcanology

2017

Ultraviolet imaging has been applied in volcanology over the last ten years or so. This provides considerably higher temporal and spatial resolution volcanic gas emission rate data than available previously, enabling the volcanology community to investigate a range of far faster plume degassing processes than achievable hitherto. To date, this has covered rapid oscillations in passive degassing through conduits and lava lakes, as well as puffing and explosions, facilitating exciting connections to be made for the first time between previously rather separate sub-disciplines of volcanology. Firstly, there has been corroboration between geophysical and degassing datasets at ≈1 Hz, expeditin…

volcanic plumes010504 meteorology & atmospheric sciencesLavaEarth scienceFlow (psychology)010502 geochemistry & geophysicsmedicine.disease_cause01 natural sciencesVolcanic plumeInterdisciplinary volcanology; Ultraviolet cameras; Volcanic plumes; Earth and Planetary Sciences (all)medicineinterdisciplinary volcanology0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryultraviolet cameraslcsh:QE1-996.5Gas releaseVolcanologyGeophysicsPlumelcsh:GeologyDynamic modelsVolcano13. Climate actionGeneral Earth and Planetary SciencesEarth and Planetary Sciences (all)GeologyUltravioletUltraviolet camera
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Evolution of Seismicity During a Stalled Episode of Reawakening at Cayambe Volcano, Ecuador

2021

Cayambe Volcano is an ice-capped, 5,790 m high, andesitic-dacitic volcanic complex, located on the equator in the Eastern Cordillera of the Ecuadorian Andes. An eruption at Cayambe would pose considerable hazards to surrounding communities and a nationally significant agricultural industry. Although the only historically documented eruption was in 1785, it remains persistently restless and long-period (LP) seismicity has been consistently observed at the volcano for over 10 years. However, the sparse monitoring network, and complex interactions between the magmatic, hydrothermal, glacial, and tectonic systems, make unrest at Cayambe challenging to interpret. In June 2016 a seismic “crisis” …

volcano-tectonic interactionsgeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesScienceEquatorQvolcano-glacier interactionsInduced seismicityFault (geology)010502 geochemistry & geophysics01 natural sciencesTectonicsVolcanoMagmavolcano-seismic swarmsGeneral Earth and Planetary SciencesGlacial periodlong-period seismicityVolcanic coneGeologySeismology0105 earth and related environmental sciencesvolcanic monitoringFrontiers in Earth Science
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Atmospheric circulation modulates the spatial variability of temperature in the Atlantic-Arctic region

2019

International audience; The Arctic region has experienced significant warming during the past two decades with major implications on the cryosphere. The causes of Arctic amplification are still an open question within the scientific community, attracting recent interest. The goal of this study is to quantify the contribution of atmospheric circulation on temperature variability in the Atlantic–Arctic region at decadal to intra‐annual timescales from 1951 to 2014. Daily 20th Century reanalyses geopotential height anomalies at 500 hPa were clustered into different weather regimes to assess their contribution to observed temperature variability. The results show that in winter, 25% of the warm…

weather regimesAtmospheric Science010504 meteorology & atmospheric sciencesreanalysesAtmospheric circulationarctic amplification[SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]atmospheric circulation0207 environmental engineeringGeopotential heightClimate changeinternal climate variability02 engineering and technology01 natural sciencesAtlantic–ArcticSea iceCryosphere020701 environmental engineeringAir mass0105 earth and related environmental sciencesgeographygeography.geographical_feature_category[SHS.GEO]Humanities and Social Sciences/GeographyArctic13. Climate action[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/ClimatologyClimatologyPolar amplificationEnvironmental science
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