Physics
Scientist
A.Holzheid, Universität Münster, Institut für Mineralogie, Corrensstr. 24, Münster, 48149 Germany für Mineralogie, Universität Münster, Corrensstrasse 24, 48149 Münster, Germany; Institut für Geowissenschaften, Universität Kiel, Ludewig-Meyn-Strasse 10, 24118 Kiel, Germany
Institut für Geowissenschaften, Universität Kiel, Kiel, D-24118, Germany
Max-Planck-Inst. für Chemie, Mainz, Germany
Bayerisches Geoinstitut, Universität Bayreuth, D-95440, Bayreuth, Germany
Mineralogisch-Petrographisches Institut, Universität zu Köln, Zulpicher Str. 49b, 50674 Köln, Germany
Institut für Geowissenschaften, Universität Kiel, D-24098 Kiel, Germany
Accretion and Core Formation of Terrestrial Planets: Insights from Experimentally Determined Solubility Behavior of Siderophile Elements in Silicate Liquids
Accretion and Early History of the Earth: Constraints Imposed by NI and CO Abundances in the Earth's Mantle
Carbonate-rich Material Associated with Meteor Crater Impact Melt Particles
Comment on "Prediction of metal-silicate partition coefficients for siderophile elements: An update and assessment of PT conditions for metal-silicate equilibrium during accretion of the Earth" by K. Righter, EPSL 304 (2011) 158-167, 2011
Cooling Rates of Porphyritic Olivine and Excentroradial Pyroxene Chondrules
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