Replication Data for: A possible high-temperature origin of the Moon and its geochemical consequences.

• 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>