The osmium isotopic ratio of Os-187/Os-188 ranging from 0.126 to 0.127
for the primitive upper mantle (PUM) is obtained according to the cor
relation between Os-187/Os-188 and Al2O3 of mantle-derived xenoliths a
nd orogenic peridotites, which consists with Allegre and Luck's ALM va
lue and similar to Yin's nuggets uniform reservoir (NUR) value. It sho
ws that the Os isotope ratio is lower than enstatite or ondinary chond
rites, similar to carbonaceous chondrites (CV3).