Data are discussed on the abundance and chemical composition of chrome
-pyrope, magnesian ilmenite, chrome-spinel, chrome-diopside, olivine,
and diamond found in alluvial deposits of modern river basins in the R
ussian Far East. A kimberlite and lamproite nature for the majority of
the minerals is indicated with 50% probability level. Complex anomali
es of indicator-minerals have been established within the structure of
different zones. These heavy mineral anomalies are treated as the mos
t promising areas for finding kimberlite and lamproite magmatism.