Late Triassic age for the Olzit bimodal suite and coeval granites.
Basaltic end-member derived from partial melting of an enriched lithospheric mantle.
Granites and rhyolitic end-member of the bimodal suite have A-type affinity.
Olzit bimodal suite and coeval granites represent a back-arc basin extension of the Mongol–Okhotsk Ocean.