Search results for "Geochemistry & geophysics"

showing 10 items of 1480 documents

Raman Investigations to Identify Corallium rubrum in Iron Age Jewelry and Ornaments

2016

International audience; During the Central European Iron Age, more specifically between 600 and 100 BC, red precious corals (Corallium rubrum) became very popular in many regions, often associated with the so-called (early) Celts. Red corals are ideally suited to investigate several key questions of Iron Age research, like trade patterns or social and economic structures. While it is fairly easy to distinguish modern C. rubrum from bone, ivory or shells, archaeologists are confronted with ancient, hence altered, artifacts. Due to ageing processes, archaeological corals lose their intensive red color and shiny surface and can easily be confused with these other light colored materials. We pr…

polyeneslcsh:QE351-399.2[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and PrehistoryDistribution networks02 engineering and technologyBiology010502 geochemistry & geophysics01 natural sciencescorals; shells; Raman spectroscopy; biogenic carbonates; carotenoids; polyenes; color fading; material degradation; archaeology[CHIM.ANAL]Chemical Sciences/Analytical chemistryArchaeological researchMaterial DegradationCorallium rubrumcoral0105 earth and related environmental sciencesmaterial degradationlcsh:MineralogyEcologycarotenoidscolor fadingGeologyOrnamentsarchaeology021001 nanoscience & nanotechnologyGeotechnical Engineering and Engineering Geologybiogenic carbonatesshellscoralsIron AgeRaman spectroscopy0210 nano-technology[SDU.STU.MI]Sciences of the Universe [physics]/Earth Sciences/MineralogyMinerals
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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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Investigation of a Gravel-Bed River’s Pattern Changes: Insights from Satellite Images

2021

Changes in river pattern have been documented in the literature. The recognition of islands and vegetated patches, which is indicative of the evolution processes, requires simultaneous information at different points and at different times and field studies are still difficult and scarce. The present work, focusing the attention on a gravel-bed river, explores the possibility to conduct a first-step pattern changes analysis by identifying the evolution of the morphological features and taking information of islands and vegetated patches from satellite images easily available from Google Earth. The study is conducted by combining the information taken from both the satellite images and the f…

river pattern010504 meteorology & atmospheric sciencesriverFlow (psychology)Flux010502 geochemistry & geophysicslcsh:Technology01 natural sciencesDeposition (geology)Settore ICAR/01 - Idraulicalcsh:ChemistryGeneral Materials Sciencelcsh:QH301-705.5Instrumentation0105 earth and related environmental sciencesFluid Flow and Transfer Processeslcsh:TProcess Chemistry and TechnologyGeneral EngineeringSedimentvegetated patcheVegetationpredictionlcsh:QC1-999Field (geography)Computer Science Applicationsimagesmonitoringlcsh:Biology (General)lcsh:QD1-999lcsh:TA1-2040morphological evolutionSatellitePhysical geographylcsh:Engineering (General). Civil engineering (General)Sediment transportlcsh:PhysicsGeologyApplied Sciences
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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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Joint second-order parameter estimation for spatio-temporal log-Gaussian Cox processes

2018

We propose a new fitting method to estimate the set of second-order parameters for the class of homogeneous spatio-temporal log-Gaussian Cox point processes. With simulations, we show that the proposed minimum contrast procedure, based on the spatio-temporal pair correlation function, provides reliable estimates and we compare the results with the current available methods. Moreover, the proposed method can be used in the case of both separable and non-separable parametric specifications of the correlation function of the underlying Gaussian Random Field. We describe earthquake sequences comparing several Cox model specifications.

spatio-temporal pair correlation functionEnvironmental EngineeringGaussianminimum contrast methodnon-separable covariance function010502 geochemistry & geophysics01 natural sciencesPoint processGaussian random fieldSet (abstract data type)010104 statistics & probabilitysymbols.namesakeCorrelation functionEnvironmental Chemistry0101 mathematicsSafety Risk Reliability and Qualityearthquakes0105 earth and related environmental sciencesGeneral Environmental ScienceWater Science and TechnologyParametric statisticsMathematicslog-Gaussian Cox processesEstimation theoryContrast (statistics)symbolsEarthquakes Log-Gaussian Cox processes Minimum contrast method Non-separable covariance function Spatio-temporal pair correlation functionSettore SECS-S/01 - StatisticaAlgorithm
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Holocene Spatiotemporal Redox Variations in the Southern Baltic Sea

2021

Low oxygen conditions in the modern Baltic Sea are exacerbated by human activities; however, anoxic conditions also prevailed naturally over the Holocene. Few studies have characterized the specific paleoredox conditions (manganous, ferruginous, euxinic) and their frequency in southern Baltic sub-basins during these ancient events. Here, we apply a suite of isotope systems (Fe, Mo, S) and associated elemental proxies (e.g., Fe speciation, Mn) to specifically define water column redox regimes through the Baltic Holocene in a sill-proximal to sill-distal transect (Lille Belt, Bornholm Basin, Landsort Deep) using samples collected during the Integrated Ocean Drilling Program Expedition 347. At…

sulfur isotopes010504 meteorology & atmospheric sciencesBaltic SeaScienceGeochemistryStructural basinengineering.material010502 geochemistry & geophysics01 natural sciencesWater columnSillHolocene0105 earth and related environmental sciencesgeographypaleoredoxgeography.geographical_feature_categorybiologyQLittorinairon isotopesbiology.organism_classificationAnoxic watersDiagenesismolybdenum isotopesengineeringGeneral Earth and Planetary SciencesPyritediagenesisGeologyFrontiers in Earth Science
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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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