Development of the geology, geochemistry, and analytical chemistry of noble metals (NM) in the past 30 years has provided new insights into the nature of unconventional complex gold and platinum group metal (PGM) deposits. In particular, such deposits confined to black shales were discovered in Caledonides of the Central Asian orogenic belt, such as the well-known Muruntau, Kumtor, Zun-Kholba, Irokinda, Sukhoi Log, Nezhdaninskoe, Natalka, and others. In the past 10‐15 years, commercial PGM concentrations were detected in ores of these deposits [1‐4 and others]. The PGMs in these deposits are traditionally assigned to the carbonaceous matter (CM) of rocks. However, it turned out that they are likely (and primarily) associated with sulfides. Geochemical aspects of PGM concentration in rocks (and ores) and issues of their reliable determination have attracted the main attention in discussions devoted to the problem of PGM occurrence in black shales in the recent period of more than 20 years [4, 5, and others]. The Khankai massif is located at the center of the Central Asian orogenic belt in the Russian Far East. The NM mineralization (Au + PGM) was recently discovered in graphitized rocks [6] of the well-known graphite deposits in the Lesozavodsk region of Primorye [7]. Relative to the typical black shales mentioned above, these rocks are almost devoid of sulfides [8]. However, this interesting feature is provoked apparently by technical difficulties in the analysis of PGMs. For example, analysis of Au and Pt by glow discharge ion mass spectrometry (GDI MS) [9] yielded 3‐30 and 4‐52 g/t, respectively. Duplicate analysis of the same samples by atomic coupled plasma atomic emission spectrometry (ICP AES) and atomic absorption spectrometry by thermoelectric atomization with prior extract concentration (EC TEA) yielded, on average, two orders of lower Au concentrations, while the presence of Pt was not confirmed at all [10]. However, such contradictory results are common for the analysis of black shales due to both poor representativeness of the samples analyzed and losses of the NM during the chemical preparation of samples and their transfer to solutions, as was demonstrated for the Natalka deposit [5, 11, and others].