about
Early solar system. Early accretion of water in the inner solar system from a carbonaceous chondrite-like sourceNominally hydrous magmatism on the Moon.Unique meteorite from early Amazonian Mars: water-rich basaltic breccia Northwest Africa 7034.Early accretion of water and volatile elements to the inner Solar System: evidence from angrites.The origin of water in the primitive Moon as revealed by the lunar highlands samplesRb-Sr and Sm-Nd isotopic and REE studies of igneous components in the bulk matrix domain of Martian breccia Northwest Africa 7034A review of volatiles in the Martian interiorRapid post-mortem maturation of diatom silica oxygen isotope valuesApatites in lunar KREEP basalts: The missing link to understanding the H isotope systematics of the MoonHydrous melting of the martian mantle produced both depleted and enriched shergottitesHydrothermal jarosite and hematite in a pyroxene-hosted melt inclusion in martian meteorite Miller Range (MIL) 03346: Implications for magmatic-hydrothermal fluids on MarsThe potential for metal contamination during Apollo lunar sample curationSilica-rich volcanism in the early solar system dated at 4.565 GaGeologic history of Martian regolith breccia Northwest Africa 7034: Evidence for hydrothermal activity and lithologic diversity in the Martian crustEarly degassing of lunar urKREEP by crust-breaching impact(s)Experimental investigation of F, Cl, and OH partitioning between apatite and Fe-rich basaltic melt at 1.0–1.2 GPa and 950–1000 °CPetrology of igneous clasts in Northwest Africa 7034: Implications for the petrologic diversity of the martian crustMagmatic volatiles (H, C, N, F, S, Cl) in the lunar mantle, crust, and regolith: Abundances, distributions, processes, and reservoirsAnalysis of MESSENGER high-resolution images of Mercury's hollows and implications for hollow formationEarly loss, fractionation, and redistribution of chlorine in the Moon as revealed by the low-Ti lunar mare basalt suiteThe Northwest Africa 8159 martian meteorite: Expanding the martian sample suite to the early AmazonianA Low O/Si Ratio on the Surface of Mercury: Evidence for Silicon Smelting?Heterogeneous distribution of H2 O in the Martian interior: Implications for the abundance of H2 O in depleted and enriched mantle sourcesThe provenance, formation, and implications of reduced carbon phases in Martian meteoritesFluorine and chlorine abundances in lunar apatite: Implications for heterogeneous distributions of magmatic volatiles in the lunar interiorGeochemistry, mineralogy, and petrology of boninitic and komatiitic rocks on the mercurian surface: Insights into the mercurian mantleChlorine on the surface of Mercury: MESSENGER gamma-ray measurements and implications for the planet’s formation and evolutionMultiple reservoirs of volatiles in the Moon revealed by the isotopic composition of chlorine in lunar basaltsThe oxidation state of sulfur in lunar apatiteIs Mercury a volatile-rich planet?Reclassification of four aubrites as enstatite chondrite impact melts: Potential geochemical analogs for Mercury
P50
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P50
name
Francis M. McCubbin
@en
Francis M. McCubbin
@nl
type
label
Francis M. McCubbin
@en
Francis M. McCubbin
@nl
prefLabel
Francis M. McCubbin
@en
Francis M. McCubbin
@nl