dc.creator
Steenstra, E. S.
dc.creator
Berndt, Jasper
dc.creator
Westrenen, W. van
dc.identifier
https://doi.org/10.35003/I8TSNK
dc.description
• Core-mantle distribution of many elements was studied for lunar melt compositions.<br>
• Depletions of Co and Ni provide evidence for a giant-impact origin of the Moon.<br>
• Most volatile siderophile elements (VSE) do not behave strongly siderophile at high temperatures.<br>
• Lunar mantle depletions of most VSE require significant volatility-related loss.<br>
dc.subject
Element core-mantle distribution
dc.subject
Depletions of Co and N
dc.subject
Volatile siderophile elements (VSE)
dc.subject
Lunar mantle depletions of VSE
dc.title
Replication Data for: A possible high-temperature origin of the Moon and its geochemical consequences.
