Chromites are a common component of the heavy fraction of sedimentary deposits of the cover of the platform areas, while their contents usually do not exceed the first percent. Placers of chromites of economic importance, as a rule, are formed in close connection of indigenous sources. Within the Lukoyanovsky placer area (Nizhny Novgorod region), high chromite contents (up to 100 kg/m3) were found in complex coastal-marine rare metal-titanium placers of the Middle Jurassic system, which is of economic importance. Placer bodies are localized on the periphery of the domed structures of the sedimentary cover. A possible source is the Upper Permian and Lower Jurassic sediments, which were eroded in the zone of positive tectonic structures of the cover and foundation of the platform and within the adjacent land. The studied patterns can serve as a basis for forecasting similar deposits within promising areas.
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