0000000000280433

AUTHOR

Olivier Alard

0000-0002-0832-6625

showing 3 related works from this author

MPI-DING reference glasses for in situ microanalysis: New reference values for element concentrations and isotope ratios

2006

We present new analytical data of major and trace elements for the geological MPI-DING glasses KL2-G, ML3B-G, StHs6/80-G, GOR128-G, GOR132-G, BM90/21-G, T1-G, and ATHO-G. Different analytical methods were used to obtain a large spectrum of major and trace element data, in particular, EPMA, SIMS, LA-ICPMS, and isotope dilution by TIMS and ICPMS. Altogether, more than 60 qualified geochemical laboratories worldwide contributed to the analyses, allowing us to present new reference and information values and their uncertainties (at 95% confidence level) for up to 74 elements. We complied with the recommendations for the certification of geological reference materials by the International Associ…

In situ010504 meteorology & atmospheric sciencesIsotopeTrace elementMineralogyElectron microprobeIsotope dilution010502 geochemistry & geophysics01 natural sciencesMicroanalysisGeophysics13. Climate actionGeochemistry and PetrologyReference valuesGeology0105 earth and related environmental sciencesGeochemistry, Geophysics, Geosystems
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Melting of sediments in the deep mantle produces saline fluid inclusions in diamonds.

2019

We demonstrate the formation of highly saline mantle fluids by the reaction of subducted sediment with peridotite.

[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and Prehistory010504 meteorology & atmospheric scienceseducationGeochemistry[SDU.STU]Sciences of the Universe [physics]/Earth Sciencesengineering.material010502 geochemistry & geophysics01 natural sciencesMantle (geology)[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryLithosphereFluid inclusionsResearch Articles0105 earth and related environmental sciencesPeridotiteMultidisciplinarySubductionDiamondSciAdv r-articlesGeologyGeochemistry13. Climate action[SDE]Environmental SciencesengineeringMicaKimberliteGeologyResearch ArticleScience advances
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Partitioning of nitrogen during melting and recycling in subduction zones and the evolution of atmospheric nitrogen

2019

Abstract The subduction of sediment connects the surface nitrogen cycle to that of the deep Earth. To understand the evolution of nitrogen in the atmosphere, the behavior of nitrogen during the subduction and melting of subducted sediments has to be estimated. This study presents high-pressure experimental measurements of the partitioning of nitrogen during the melting of sediments at sub-arc depths. For quantitative analysis of nitrogen in minerals and glasses, we calibrated the electron probe micro-analyzer on synthetic ammonium feldspar to measure nitrogen concentrations as low as 500 μg g−1. Nitrogen abundances in melt and mica are used together with mass balance calculations to determi…

010504 meteorology & atmospheric sciencesAnalytical chemistrychemistry.chemical_element[SDU.STU]Sciences of the Universe [physics]/Earth Sciences010502 geochemistry & geophysicsFeldspar01 natural sciencesMantle (geology)Geochemistry and Petrology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistrySubduction zonesNitrogen cycle0105 earth and related environmental sciencesMantle metasomatismSubductionGeologyNitrogenPartition coefficientchemistry13. Climate action[SDU]Sciences of the Universe [physics]visual_art[SDE]Environmental Sciencesvisual_art.visual_art_mediumSlabAtmosphere evolutionMicaGeologyNitrogen cycling
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