We present results of siderophile-element analysis of two FeNi metal grains from the Apollo 16 regolith which each likely crystallized from an impact melt. One is unusual in having a high Ir/Au ratio and high Ga concentration for Apollo 16 metal.
Siderophile Element Concentrations in Two Metal Fragments from the Apollo 16 Regolith
2000-03-01
Conference paper
No indication
English
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