We report the first noble gas isotopic compositions of peridotites from Patagonia.
Pali-Aike mantle xenoliths represent an extensively degassed and intrinsic SCLM.
SCLM shows high 4He/3He = 104000, 21Ne/22Ne(E) = 0.09, and 40Ar/36Ar(E) = 54000.
MORB-like metasomatism could be explained by recent slab window beneath Patagonia.
Pali-Aike SCLM have, at least, a similar excess of 129Xe and 136Xe to that of MORB.