Stachel T.; Tappert R.; Aulbach S.; Brey G.P.; Leost I.; Harris J.W.; Viljoen K.S.
(2004)
On a global scale, peridotitic garnet inclusions in diamonds from the subcratonic lithosphere indicate an evolution from strongly sinusoidal REEN, typical for harzburgitic garnets, to mildly sinusoidal or “normal” patterns ...