IN the eastern part of the Aldansky shield, on the territory of volcanic and sedimentary basins of Proterozoic age, many deposits and ore occurrences of Au, Ag, Mo, U, V, Ni, Co, Ba and Th are revealed.Petrographic, geochemical and fluid inclusion study indicate their low temperature (epithermal) genesis.It is supposed that these ores were formed in the grenville metallogenic epoch (Upper Proterozoic). The epithermal ores in this region are connected with: (i) eisite (apatite-albite metasomatites)and (ii) argilliceous-white mica metasomatites (argillisites and beresites). Apatite-albite metasomatitesare associated with rare-earth ores. As a rule, metasomatite bodies are controlled by steeply-dipping fractures. Albite, quartz and fine-grained hematite form a typical mineral assiciation. The ore bearing metasomatites were formed at pH = 4 and T≤300℃. The beresite type argillaceous-white mica alterations are widespread in volcanic rocks of the Ulkansky basin and in the sedimentary suites of the Uchursky basin. They are distinguished on all stratigraphiclevels, but especially often in a zone of structural-stratigraphic unconformity (SSU) of AR-PR. Au, Ag,Mo, V and U deposits and occurrences are connected with this type of alterations. Their structural pos- IN the eastern part of the Aldansky shield, on the territory of volcanic and sedimentary basins of Proterozoic age, many deposits and ore occurrences of Au, Ag, Mo, U, V, Ni, Co, Ba and Th are revealed. Petrographic, geochemical and fluid inclusion study indicate their low temperature (epithermal) genesis. It is said that these ores were formed in the grenville metallogenic epoch (Upper Proterozoic). The epithermal ores in this region are connected with: (i) eisite (apatite-albite metasomatites ) and (ii) argilliceous-white mica metasomatites (argillisites and beresites). Apatite-albite metasomatitesare associated with rare-earth ores. As a rule, metasomatite bodies are controlled by steeply-dipping fractures. Albite, quartz and fine-grained hematite form a typical mineral assemblage. The ore bearing metasomatites were formed at pH = 4 and T <300 ° C. The beresite type argillaceous-white mica alterations are widespread in volcanic rocks of the Ulkansky basin and in the sedimentary sui testes of the Uchursky basin. They are distinguished on all stratigraphiclevels, but especially often in a zone of structural-stratigraphic unconformity (SSU) of AR-PR. Au, Ag, Mo, V and U deposits and occurrences are connected with this type of of alterations. Their structural pos-