about
Evaporative fractionation of volatile stable isotopes and their bearing on the origin of the MoonZinc isotopic evidence for the origin of the MoonEarly formation of evolved asteroidal crust.Extensive volatile loss during formation and differentiation of the MoonLate-stage magmatic outgassing from a volatile-depleted MoonEvaporative fractionation of zinc during the first nuclear detonationIsotopic links between atmospheric chemistry and the deep sulphur cycle on MarsStochastic late accretion to Earth, the Moon, and MarsHighly siderophile element constraints on accretion and differentiation of the Earth-Moon systemTungsten-182 heterogeneity in modern ocean island basaltsAnomalous sulphur isotopes in plume lavas reveal deep mantle storage of Archaean crustHalogens in chondritic meteorites and terrestrial accretion.Earth science: Extraordinary worldHadean silicate differentiation preserved by anomalous 142Nd/144Nd ratios in the Réunion hotspot sourceSubducted oceanic crust as diamond hosts revealed by garnets of mantle xenoliths from Nyurbinskaya, SiberiaHelium isotopic evidence for modification of the cratonic lithosphere during the Permo-Triassic Siberian flood basalt eventThe helium flux from the continents and ubiquity of low-3He/4He recycled crust and lithosphereHelium isotope evidence for a deep-seated mantle plume involved in South Atlantic breakupPyroxenite-rich mantle formed by recycled oceanic lithosphere: Oxygen-osmium isotope evidence from Canary Island lavasAbsence of a high time-integrated 3He/(U+Th) source in the mantle beneath continentsA sulfide perspective on iron isotope fractionation during ocean island basalt petrogenesisMartian magmatism from plume metasomatized mantle1.34 billion-year-old magmatism on Mars evaluated from the co-genetic nakhlite and chassignite meteoritesChondritic late accretion to Mars and the nature of shergottite reservoirsThe potential for metal contamination during Apollo lunar sample curationEvidence against an ancient non-chondritic mantle source for North Atlantic Igneous Province lavasEarly mantle heterogeneities in the Réunion hotspot source inferred from highly siderophile elements in cumulate xenolithsHighly siderophile element depletion in the MoonHotspot volcanism and highly siderophile elementsChemical heterogeneity in the upper mantle recorded by peridotites and chromitites from the Shetland Ophiolite Complex, ScotlandEvolution of the martian mantle inferred from the 187Re–187Os isotope and highly siderophile element abundance systematics of shergottite meteoritesLate accretion as a natural consequence of planetary growthOrigin of felsic achondrites Graves Nunataks 06128 and 06129, and ultramafic brachinites and brachinite-like achondrites by partial melting of volatile-rich primitive parent bodiesOxygen isotope heterogeneity of the mantle beneath the Canary Islands: a discussion of the paper of Gurenko et alPlanetary-Scale Strontium Isotopic Heterogeneity and the Age of Volatile Depletion of Early Solar System MaterialsRhenium–osmium isotope and highly-siderophile-element abundance systematics of angrite meteoritesEvidence for heterogeneous enriched shergottite mantle sources in Mars from olivine-hosted melt inclusions in Larkman Nunatak 06319Helium isotope variations between Réunion Island and the Central Indian Ridge (17°–21°S): New evidence for ridge–hot spot interactionErratum to “Rhenium–osmium isotopes and platinum-group elements in the Rum Layered Suite, Scotland: Implications for Cr-spinel seam formation and the composition of the Iceland mantle anomaly” [Earth and Planetary Science Letters 286 (2009) 41?A laser-ablation ICP-MS study of Apollo 15 low-titanium olivine-normative and quartz-normative mare basalts
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description
Geoscientist
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onderwijzer
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James M.D. Day
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James M.D. Day
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James M.D. Day
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James M.D. Day
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James M.D. Day
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James M.D. Day
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James M.D. Day
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James M.D. Day
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James Day
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James M D Day
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James M. D. Day
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James MD Day
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James M.D. Day
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James M.D. Day
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James M.D. Day
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James M.D. Day
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