Аннотация:Various new-generation mineral forms of carbon are widespread among tectonized sedimentary strata in Maritime Siberia where they are commonly associated with ilmenite, carbonate and sulfides. They were described earlier as graphite-ilmenite metasomatites. These report considers how these metasomatites are localized within the region, whether they are confined to specific geologic formations, and the stages of the tectonic evolution of the region. Their geochemistry is also described.