Search results for "SL"

showing 10 items of 12921 documents

Collapse of a two-dimensional brittle granular column: Implications for understanding dynamic rock fragmentation in a landslide

2015

We investigate numerically the failure, collapse and flow of a two-dimensional brittle granular column over a horizontal surface. In our discrete element simulations, we consider a vertical monolayer of spherical particles that are initially held together by tensile bonds, which can be irreversibly broken during the collapse. This leads to dynamic fragmentation within the material during the flow. Compared to what happens in the case of a non-cohesive granular column, the deposit is much rougher, and the internal stratigraphic structure of the column is not preserved during the collapse. As has been observed in natural rockslides, we find that the deposit consists of large blocks laying on …

010504 meteorology & atmospheric sciencesGeometryLandslideRockslide01 natural sciences010305 fluids & plasmasEarth surfaceGeophysicsBrittlenessFragmentation (mass spectrometry)0103 physical sciencesMonolayerUltimate tensile strengthGeotechnical engineeringGeology0105 earth and related environmental sciencesEarth-Surface ProcessesJournal of Geophysical Research: Earth Surface
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Understanding volcanoes in the Vanuatu arc

2016

We report the first helium isotope survey of volcanic gases, hot springs and some olivine phenocrysts along the Vanuatu island arc, from Tanna in the south to Vanua Lava in the north. Low CO2 content and low He-3/He-4 ratios in thermal fluids of Epi (4.0 +/- 0.1 R-a), Efate (4.5 +/- 0.1 R-a) and Pentecost (5.3 +/- 0.5 R-a) islands coherently indicate reduced mantle gas leakage and crustal contamination by radiogenic helium on these extinct volcanic systems of the former (Pliocene) arc. Instead, presently active Vanuatu volcanoes display He-3/He-4 and C/He-3 ratios typical of subduction-related volcanic arcs: He-3/He-4 ratios range from 6.4 +/- 0.5 Ra in southernmost Tanna and 7.23 +/- 0.09 …

010504 meteorology & atmospheric sciencesLavaEarth scienceGeochemistryVanuatu arcHelium isotopes[SDU.STU]Sciences of the Universe [physics]/Earth Sciences010502 geochemistry & geophysics01 natural sciencesVolcanic fluidsVolcanic GasesGeochemistry and Petrologyevent0105 earth and related environmental sciencesBasaltevent.disaster_typegeographygeography.geographical_feature_categoryVolcanic arcHotspot contributionFumaroleExtinct and active volcanoesMantle sourceSettore GEO/08 - Geochimica E VulcanologiaGeophysicsVolcano13. Climate actionVanuatu arc Volcanic fluids Helium isotopes Extinct and active volcanoes Mantle source Hotspot contributionIsland arcPhenocrystGeology
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Sustaining persistent lava lakes: Observations from high-resolution gas measurements at Villarrica volcano, Chile

2016

International audience; Active lava lakes – as the exposed upper part of magmatic columns – are prime locations to investigate the conduit flow processes operating at active, degassing volcanoes. Persistent lava lakes require a constant influx of heat to sustain a molten state at the Earth's surface. Several mechanisms have been proposed to explain how such heat transfer can operate efficiently. These models make contrasting predictions with respect to the flow dynamics in volcanic conduits and should result in dissimilar volatile emissions at the surface. Here we look at high-frequency SO2 fluxes, plume composition, thermal emissions and aerial video footage from the Villarrica lava lake i…

010504 meteorology & atmospheric sciencesLavaEarth scienceUAVUV camera010502 geochemistry & geophysics01 natural sciencesElectrical conduitFlux (metallurgy)Geochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyPetrologyGeophysic0105 earth and related environmental sciencesgeographyTrail By Firegeography.geographical_feature_categoryTrail ByLava domeFireconduit dynamicPlumeGeophysicsVolcano13. Climate actionSpace and Planetary ScienceGas slugMagmavolcanic degassingGeologyMulti-GAS
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Prodigious emission rates and magma degassing budget of major, trace and radioactive volatile species from Ambrym basaltic volcano, Vanuatu island Arc

2016

Abstract Ambrym volcano, in the Vanuatu arc, is one of the most active volcanoes of the Southwest Pacific region, where persistent lava lake and/or Strombolian activity sustains voluminous gas plume emissions. Here we report on the first comprehensive budget for the discharge of major, minor, trace and radioactive volatile species from Ambrym volcano, as well as the first data for volatiles dissolved in its basaltic magma (olivine-hosted melt inclusions). In situ MultiGAS analysis of H 2 O, CO 2 , SO 2 and H 2 S in crater rim emissions, coupled with filter-pack determination of SO 2 , halogens, stable and radioactive metals demonstrates a common magmatic source for volcanic gases emitted by…

010504 meteorology & atmospheric sciencesLavaGeochemistryMineralogy[SDU.STU]Sciences of the Universe [physics]/Earth SciencesAmbrymVolatile fluxes010502 geochemistry & geophysics01 natural sciencesVolcanic GasesMagma reservoirVanuatuVolatile fluxeGeochemistry and PetrologyCalderaeventGeophysicComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesMelt inclusionsBasaltevent.disaster_typegeographygeography.geographical_feature_categoryMagma degassing budgetStrombolian eruptionGeophysicsVolcano13. Climate actionIsland arcRadioactive disequilibriaGeology
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Geochemistry of ultramafic and mafic rocks from the northern Central Asian Orogenic Belt (Tuva, Central Asia) - constraints on lower and middle arc c…

2021

Abstract The Agardagh Tes-Chem complex (ATCC) in Tuva, Central Asia (50.5°N, 95°E) exposes a rare mafic to ultramafic crust-mantle fragment that developed within a late Neoproterozoic (~570 Ma) intra-oceanic island arc system that was accreted to the Tuva-Mongolian microcontinent during the formation of the Central Asian Orogenic Belt. Residual mantle rocks (harzburgites and dunites) are highly refractory with high Cr# (0.59–0.83) and intermediate Mg# (0.46–0.52) in spinel and experienced high degrees of total melt extraction (up to 25%). In ultramafic cumulate rocks (wehrlites and pyroxenites), Cr# and Mg# in spinel are distinctly lower (0.22–0.45 and 0.34–0.37), and rare earth element (RE…

010504 meteorology & atmospheric sciencesMantle wedgeProterozoicGeochemistryCumulate rockGeologyCrust010502 geochemistry & geophysics01 natural sciencesGeochemistry and PetrologyUltramafic rockMagmaIsland arcMaficGeology0105 earth and related environmental sciencesPrecambrian Research
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The imprint of subduction fluids on subducted MORB-derived melts (Sierra del Convento Mélange, Cuba)

2011

International audience; Major and trace element signatures and Sr-Nd-Pb isotope data for muscovite (Ms)-bearing amphibolite blocks and associated muscovite-bearing trondhjemite and quartz-muscovite rocks from the Sierra del Convento melange (eastern Cuba) indicate that Proto-Caribbean oceanic crust underwent wet partial melting processes during Mesozoic subduction and after accretion to the upper plate. Trace element normalized patterns of Ms-bearing amphibolites are enriched in light rare earth elements (LREE) and large-ion lithophile elements (LILE) and evidence variable trace element transfer from the Proto-Caribbean subducting slab to the mantle wedge. Ms-bearing trondhjemites show LREE…

010504 meteorology & atmospheric sciencesMantle wedge[SDE.MCG]Environmental Sciences/Global ChangesFluid compositionTrondhjemiteGeochemistrySedimentary imprint010502 geochemistry & geophysics01 natural sciences[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryGeochemistry and PetrologyOceanic crust0105 earth and related environmental sciencesBasaltTrace elementsSubductionbiologyPartial meltingTrace elementGeologySr-Nd-Pb isotopesbiology.organism_classification13. Climate actionAdakiteLileGeologySlab meltsLithos
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Strain rate dependence for evolution of steady state grain sizes: Insights from high-strain experiments on ice

2019

Abstract Understanding of the microstructural evolution and equilibrium grain size development during steady state tertiary flow is essential in order to improve our knowledge of ice and rock deformation. This contribution presents results from in situ transmitted light deformation experiments of natural glacier ice, with the development of the microstructure in a tertiary flow regime. We conducted one relative slower ( 1 × 10 − 6 1/s) and two relative faster-strain rate ( 2 × 10 − 6 1/s) pure shear experiments at −10 °C, up to a shortening of ∼57%. Microstructure development was followed by time-lapse observations, and two new microstructure-based indicators, the ‘seeding rate’ and the ‘mi…

010504 meteorology & atmospheric sciencesMechanicsSlip (materials science)Pure shearStrain rate010502 geochemistry & geophysicsMicrostructure01 natural sciencesGrain sizeGeophysicsSpace and Planetary ScienceGeochemistry and PetrologyParticle-size distributionEarth and Planetary Sciences (miscellaneous)SeedingGeology0105 earth and related environmental sciencesStress concentrationEarth and Planetary Science Letters
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Hydrochemical mercury distribution and air-sea exchange over the submarine hydrothermal vents off-shore Panarea Island (Aeolian arc, Tyrrhenian Sea)

2017

Abstract There is a growing concern about the mercury (Hg) vented from submarine hydrothermal fluids to the marine surrounding and exchange of dissolved gaseous mercury (DGM) between the sea surface and the atmosphere. A geochemical survey of thermal waters collected from submarine vents at Panarea Island (Aeolian Islands, southern Italy) was carried out in 2015 (15–17th June and 17–18th November), in order to investigate the concentration of Hg species in hydrothermal fluids and the vertical distribution in the overlying water column close to the submarine exhalative area. Specific sampling methods were employed by Scuba divers at five submarine vents located along the main regional tecton…

010504 meteorology & atmospheric sciencesMineralogychemistry.chemical_element010501 environmental sciencesOceanographyAir-sea exchange01 natural sciencesHydrothermal circulationWater columnEnvironmental ChemistryHydrothermal fluidMercury evasion0105 earth and related environmental sciencesWater Science and TechnologySubmarineGeneral ChemistryDissolved gaseous mercuryDilutionMercury (element)Hydrothermal fluidschemistryEnvironmental chemistryAeolian processesSeawaterDissolved gaseous mercury; Mercury evasion; Air-sea exchange; Hydrothermal fluids; Panarea IslandPanarea IslandGeologyHydrothermal ventMarine Chemistry
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Sr/Ca and Mg/Ca ratios of ontogenetically old, long-lived bivalve shells (Arctica islandica) and their function as paleotemperature proxies

2011

International audience; The Sr/Ca and Mg/Ca ratios of many biogenic skeletons provide useful paleotemperature estimates. As yet however, it has remained largely impossible to obtain such information from bivalve shells. In the present study, metal-to-calcium values in the hinge plate (aragonite, outer shell layer) of four ontogenetically old (85 to 374 year-old) specimens of the long-lived bivalve, Arctica islandica, were measured on a LA-ICP-MS. The shells were collected alive in 1868, 1986 and 2003 from three different localities around Iceland. With increasing ontogenetic age and decreasing growth rate, a distinct trend toward increasing Sr/Ca (max. 5.17 mmol/mol) and Mg/Ca values (max. …

010504 meteorology & atmospheric sciencesOntogenySea surface temperatureLongevityZoologyMineralogyAmbient waterengineering.materialSignificant negative correlation010502 geochemistry & geophysicsOceanography01 natural sciencesMetal-to-calcium ratioMole14. Life underwaterGrowth rateBivalve shellArctica islandicaEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesVital effectbiologyAragonitePaleontologybiology.organism_classificationBivalve shell[SDE]Environmental Sciencesengineering
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Zipper junctions: A new approach to the intersections of conjugate strike-slip faults

2016

Intersecting pairs of simultaneously active faults with opposing slip sense present geometrical and kinematic problems. Such faults rarely offset each other but usually merge into a single fault, even when they have displacements of many kilometers. The space problems involved are solved by lengthening the merged fault (zippering up the conjugate faults) or splitting it (unzippering). This process can operate in thrust, normal, and strike-slip fault settings. Examples of conjugate pairs of large-scale strike-slip faults that may have zippered up include the Garlock and San Andreas faults in California (USA), the North and East Anatolian faults (Turkey), the Karakoram and Altyn Tagh faults (…

010504 meteorology & atmospheric sciencesOutcropGeologyThrustKinematicsActive faultSlip (materials science)010502 geochemistry & geophysicsStrike-slip tectonics01 natural sciencesShear zoneGeologySeismology0105 earth and related environmental sciencesConjugateGeology
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