Garnet peridotite of Malyi Khingan and precious metal mineralization

The stock of garnet peridotite called Taragaiskii was originally discovered on Malyi Khingan in the eastern part of the Sutarskii mountain ridge, on the northern side of Taragai Mountain, in the valley of the Kamenistyi Brook, right tributary of the Bira River. It intrudes the Early Paleozoic granite massif of the Biro bidzhan Complex in the zone of contact between the latter and metamorphosed carbonate deposits of the Murandavskaya Suite, which is included in the com position of the Late Proterozoic Khinganskii terrige nouscarbonate complex of the Malokhinganskii terrain .