about
Tracing the ingredients for a habitable earth from interstellar space through planet formation.Fe-carbonyl is a key player in planetary magmasCarbon-dioxide-rich silicate melt in the Earth's upper mantle.Structure and speciation in hydrous silica melts. 1. Temperature and composition effects.Ironing Out the Oxidation of Earth's MantleStructure and Speciation in Hydrous Silica Melts. 2. Pressure EffectsA wet mantle conductor?Melting in the Earth's deep upper mantle caused by carbon dioxideLength scales of mantle heterogeneities and their relationship to ocean island basalt geochemistryHigh-pressure partial melting of garnet pyroxenite: possible mafic lithologies in the source of ocean island basaltsHydrogen concentration analyses using SIMS and FTIR: Comparison and calibration for nominally anhydrous mineralsReading garnet's signatureMelt pathways in the mantleActivities of nickel, cobalt, and manganese silicates in magmatic liquids and applications to olivine/liquid and to silicate/metal partitioningOrigin of the Transgressive granophyres from the Layered Series of the Skaergaard intrusion, East Greenland
P50
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P50
description
onderzoeker
@nl
researcher ORCID ID = 0000-0003-1213-6645
@en
name
Marc Hirschmann
@en
Marc Hirschmann
@es
marc Hirschmann
@ast
marc Hirschmann
@nl
type
label
Marc Hirschmann
@en
Marc Hirschmann
@es
marc Hirschmann
@ast
marc Hirschmann
@nl
prefLabel
Marc Hirschmann
@en
Marc Hirschmann
@es
marc Hirschmann
@ast
marc Hirschmann
@nl
P1053
B-9455-2016
P106
P21
P31
P3829
P496
0000-0003-1213-6645