Search results for "MELT"

showing 10 items of 435 documents

Historical mining and smelting in the Vosges Mountains (France) recorded in two ombrotrophic peat bogs

2010

Two peat sequences were sampled in the vicinity of the main mining districts of the Vosges Mountains: Sainte-Marie-aux-Mines and Plancher-les-Mines. Lead isotopic compositions and excess lead fluxes were calculated for each of these radiocarbon-dated sequences. Geochemical records are in very good agreement with the mining history of the area, well known over the last millennium. Except for an anomaly corresponding to the Middle Bronze Age which has not yet been resolved, there is no clear geochemical evidence of local metal production in the Vosges before the 10th century as excess lead deposition archived between 500 BC and 500 AD is attributed to long-range transport of polluted particul…

Peat010504 meteorology & atmospheric sciencesGeochemistryOmbrotrophic010501 environmental sciencesEnvironment01 natural sciencesMiningVosgesGeochemistry and PetrologyBronze AgeGeomorphologyBog0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryMetalPeatParticulatesPollution[SDE.ES]Environmental Sciences/Environmental and SocietyArchaeological evidenceLead isotopesDeposition (aerosol physics)GeochemistryArchaeologySmeltingEconomic GeologyGeology[ SDE.ES ] Environmental Sciences/Environmental and SocietyMedieval
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Diet and prey size spectrum of pikeperch in lakes in central Finland

2004

The stomach content of pikeperch Sander lucioperca was studied in 24 lakes in central Finland. The most important prey species was smelt Osmerus eperlanus then perch Perca fluviatilis. The proportion of cyprinids as prey increased with pikeperch total length (LT) and lake phosphorus content. Prey L T and pikeperch L T correlated positively, but the prey-to-predator size ratio correlated negatively with pikeperch L T .

PerchbiologyEcologyPhosphorusZoologychemistry.chemical_elementAquatic Sciencebiology.organism_classificationPredationchemistrySize ratioOsmerus eperlanusSmeltEcology Evolution Behavior and SystematicsJournal of Fish Biology
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Gastric evacuation rate of burbot fed single-fish meals at different temperatures

1997

The gastric evacuation rates of burbot Lota lota, fed a single meal of vendace, Coregonus albula, were measured in the laboratory at five temperatures (1·3, 2·6, 4·8, 9·4 and 12·6° C). Gastric evacuation rate increased exponentially with increasing temperatrure, but the results suggest that gastric evacuation rates of burbot at low temperatures are lower than those of other freshwater fish species. Temperature and the ratio of meal weight to burbot weight were the most important factors affecting gastric evacuation rate. There was no significant difference in gastric evacuation rate between three different prey species: vendace, perch Perca fluviatilis, and smelt Osmerus eperlanus.

PerchbiologyGastric emptyingbusiness.industrydigestive oral and skin physiologyAquatic ScienceGadidaebiology.organism_classificationFisheryAnimal scienceAquacultureFreshwater fishCoregonus albulaOsmerus eperlanusbusinessSmeltEcology Evolution Behavior and SystematicsJournal of Fish Biology
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Tertiary Ultrapotassic Volcanism in Serbia: Constraints on Petrogenesis and Mantle Source Characteristics

2005

The Serbian province of Tertiary ultrapotassic volcanism is related to a post-collisional tectonic regime that followed the closure of the Tethyan Vardar Ocean by Late Cretaceous subduction beneath the southern European continental margin. Rocks of this province form two ultrapotassic groups; one with affinities to lamproites, which is concentrated mostly in the central parts of the Vardar ophiolitic suture zone, and the other with affinities to kamafugites, which crops out in volcanoes restricted to the western part of Serbia. The lamproitic group is characterized by a wide range of Sr/Sri (0 70735–0 71299) and Nd/Ndi (0 51251–0 51216), whereas the kamafugitic group is isotopically more ho…

Peridotite010504 meteorology & atmospheric sciencesGeochemistryPartial melting550 - Earth sciencesengineering.materialGeodynamics010502 geochemistry & geophysics01 natural sciencesMantle (geology)Geophysics13. Climate actionGeochemistry and PetrologyUltramafic rockengineeringPhlogopiteMetasomatismGeology0105 earth and related environmental sciencesPetrogenesisJournal of Petrology
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Origin and crystallization history of Permian tholeiites from the Saar-Nahe trough, SW Germany

1973

The Hirschberg and Rodern diatremes, within the Permian Saar-Nahe trough, SW Germany, are composed chiefly of basaltic tuffs, with associated small intrusions of K-rich tholeiites. Several tholeiite bodies carry 2–20 mm crystals of magnesian clinopyroxene and orthopyroxene, the latter containing up to 5.5% Al2O3 and often extensively resorbed and rimmed by fine-grained olivine and clinopyroxene. Experimental duplication of these pyroxenes has been achieved under conditions of Pload=6–10 kb, T=1280–1080° C and 2–4 wt.-% H2O, confirming that they represent a rare occurence of high pressure phenocrysts in tholeiitic basalts. These conditions of pyroxene crystallization also place constraints o…

PeridotiteBasaltGeophysicsSubductionGeochemistry and PetrologyContinental crustPartial meltingGeochemistryPhenocrystPyroxeneGeologyMantle (geology)Contributions to Mineralogy and Petrology
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Melt evolution beneath a rifted craton edge: 40Ar/39Ar geochronology and Sr-Nd-Hf-Pb isotope systematics of primitive alkaline basalts and lamprophyr…

2016

A new high-precision Ar-40/Ar-39 anorthoclase feldspar age of 176.7 +/- 0.5 Ma (2-sigma) reveals that small-volume alkaline basaltic magmatism occurred at the rifted SW margin of the Baltic Shield in Scania (southern Sweden), at a time of global plate reorganization associated with the inception of Pangea supercontinent break-up. Our combined elemental and Sr-Nd-Hf-Pb isotope dataset for representative basanite and nephelinite samples (>8 wt.% MgO) from 16 subvolcanic necks of the 30 by 40 km large Jurassic volcanic field suggests magma derivation from a moderately depleted mantle source (Sr-87/(86)Sri = 0.7034-0.7048; epsilon Nd-i = +4.4 to +5.2; epsilon Hf-i = +4.7 to +8.1; Pb-206/(204)Pb…

PeridotiteBasaltIncompatible elementgeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesGeochemistryPartial melting010502 geochemistry & geophysics01 natural sciencesMantle (geology)CratonMantle convectionGeochemistry and PetrologyBaltic ShieldGeology0105 earth and related environmental sciences
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The composition of near-solidus melts of peridotite in the presence of CO2 and H2O between 40 and 60 kbar

2009

Abstract Partial melting experiments at 40, 50 and 60 kbar pressure on three peridotite compositions with 0.5–0.63 wt.% H2O and 2.0–3.2 wt.% CO2 added indicate melting temperatures only marginally above continental geotherms. Most experiments were performed on a composition with 1.5 wt.% K2O added, which causes a further decrease of about 40 °C in melting temperature. Melts progress gradually from carbonate-rich to carbonated silicate in composition: near-solidus melts have Ca/(Ca + Mg) of 0.46–0.53, which fall to  30 wt.%) and Al2O3 (  9 wt.%) and concomitant decrease in CaO (> 20 to Partial melts of peridotite with CO2 and H2O are too low in MgO to resemble kimberlites, but will act as ef…

PeridotitePartial meltingGeochemistryGeologySolidusSilicatechemistry.chemical_compoundchemistryGeochemistry and PetrologyUltramafic rockMetasomatismKimberliteChemical compositionGeologyLithos
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Geodynamic Setting of the Tertiary Hocheifel Volcanism (Germany), Part II: Geochemistry and Sr, Nd and Pb Isotopic Compositions.

2007

Major and trace element as well as isotopic compositions on 26 volcanic rocks from the Tertiary Hocheifel volcanic field and for comparison from Upper Rhine Graben occurrences (western Central European Volcanic Province) were measured in order to provide geochemical evidence for the geodynamic setting of the Tertiary Eifel volcanism. Except for a few differentiated lavas there are mainly basanitic compositions. These rocks were produced by low degree partial melting of a previously metasomatized garnet peridotite source at pressures and temperatures corresponding to depths of about 75 to 90 km. In contrast to the differentiated lavas, most of the basanites are not significantly affected by …

Peridotitegeographygeography.geographical_feature_categoryPartial meltingGeochemistryMantle plumeMantle (geology)Volcanic rockGrabenVolcano[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryGeochronology[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyPetrologyGeologyComputingMilieux_MISCELLANEOUS
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Designing fluorous domains. Synthesis of a series of pyridinium salts bearing a perfluoroalkylated azole moiety

2006

The synthesis of a series of N-methylpyridinium salts bearing a perfluoroalkylated 1,2,4-oxadiazole or 1,2,4-triazole moiety is reported. X-Ray structures of representative perfluoroalkyl-triazolylpyridine (15) and methyl- pyridinium iodide salt (5a) are reported. Their crystal packing clearly shows segregation between the aromatic and parallel double layer fluorinated regions.

PharmacologyDouble layer (biology)chemistry.chemical_classificationMELTSCRYSTALChemistryDERIVATIVESPHOTOCHEMISTRYOrganic ChemistryFLUORINATED HETEROCYCLIC-COMPOUNDS124-TriazoleEXPEDIENT ROUTEAnalytical ChemistryCrystalIodide saltchemistry.chemical_compoundLIGHTIONIC LIQUIDSOXADIAZOLEPolymer chemistryMoietyOrganic chemistryAzolePyridiniumPOLYMERS
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Dielectric investigations of pure and mixed fluorocarbons in their condensed phases

1991

We review recent work and present new results on the liquid and solid fluocarbons CMF3 with M = H, F, Cl, Br, CH3, and CF3. The pure compounds as well as several series of binary mixtures were investigated using dielectric measurements. The permittivities of the non-hydrogenatcd non-polar and polar liquids could be described using the Clausius-Mosotti and the Onsager equation, respectively. In CHF3 and C2H3F3 hydrogen bridging leads to deviations from this simple behavior. The trends in the miscibility of four series of fluorocarbon mixtures are in qualitative accord with regular solution theory. The geometrical shapes of the compounds dominate the degrees of order below their melting point…

Phase transitionChemistryThermodynamicsDielectricCondensed Matter PhysicsMiscibilityAtomic and Molecular Physics and OpticsElectronic Optical and Magnetic MaterialsDipoleMaterials ChemistryMelting pointPhysical chemistryDielectric lossFluorocarbonOnsager reciprocal relationsPhysical and Theoretical ChemistrySpectroscopy
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