“…The determination of PGEs in geological materials is difficult because of their low abundance and heterogeneous distributions and the complexity of sample preparation. Methods for dissolving geological samples and thereby for concentrating PGEs include nickel sulfide (NiS) fire assay coupled with Te coprecipitation (Jackson et al, 1990;Zhou et al, 2001;Gros et al, 2002;Juvonen et al, 2002;Sun and Sun, 2005), acid attack combined with Na 2 O 2 fusion (Morgan and Walker, 1989;Yi and Masuda, 1996;Dai et al, 2001;Qi et al, 2003Qi et al, , 2004, aqua regia dissolution in a sealed Carius tube, and high pressure asher (HPA-S) (Shirey and Walker, 1995;Cohen and Waters, 1996;Rehkämper et al, 1998;Pearson and Woodland, 2000;Brauns, 2001;Meisel et al, 2001Meisel et al, , 2003aMeisel et al, , 2003bPretorius et al, 2003;Meisel and Moser, 2004). The advantages and disadvan-bration between spikes and samples.…”