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  In order to identify schlich halos selected schlich samples, which are fixed by volume or mass of loose rocks, taken from a clay-gravel-sand material. When washing in water with a tray or other devices from schlich samples extracted concentrate of heavy minerals, called concentrates. Concentrate mainly consists of heavy rock forming minerals and accessory minerals indigenous rocks, among which the ore regions observed grains of minerals.
Schlich halos are formed among the rocks of different genetic types. In areas with undivided, aligned relief eluvium enriched ore material, and there are residual mechanical ghosting, bordering the ore output and having the character of the marketplace. Detrital material is not sorted, heterogeneous granulometric composition, often contain fragments of ore or splices.
In the dissected relief weathering products shifted from primary sources, and schlich anomalies recorded in the slope or channel alluvium formations. In these cases appear displaced or separated mechanical ghosting, who lose their direct spatial relationship with a primary source and can be removed from it a considerable distance. To offset the anomalies are often typical elongated in the direction of lowering the terrain shape and a gradual transition in the linearly elongated leakage fluxes, subject to the hydrographic network. With the removal of debris material from the indigenous source increases the degree of sorting and rounding, is the disclosure of adhesions and release of mineral grains. In alluvial flows are further refinement of the mineral grains until they complete spraying in the peripheral areas of the anomalies. It should be emphasized that the ability of minerals remain in schlich anomalies is a function of the interaction of hydrodynamic factor, the physical parameters of minerals and their morphological features.