『Abstract
　The upper Amur region comprises weathering crusts (waste mantle developed at copper-nickel sulfide deposits included), which appreciably hamper the prospecting for such deposits. In order to develop their prospecting criteria, the composition of linear weathering crusts above a nickeliferous cortlandite dike and barren pyroxenite dike, as well as in the fracture zone above metamorphic rocks, was investigated. The chemical composition of material in the weathering crust and the mineral composition of newly formed clay fractions and heavy concentrate were determined. It was established that weathering crust in the nickeliferous cortlandite dike is characterized by the prevalence of fine jarosite fraction with crystobalite admixture. The heavy concentrate samples contain jarosite along with a small amount of relict sulfides (pyrite and galena) and native gold. These criteria can be used in the prospecting for copper-nickel sulfide mineralization in the upper Amur region and other similar regions.』

(Introduction)
Geological setting of the studied objects
Methods
Results
Discussion
Conclusions
References