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| At the heart of schlich method of searching is the notion of exogenous dispersion halos formed under the influence of mechanical, physical, chemical and nutrient factors and associated with the processes of weathering and denudation. When searching for schlich identify and examine the largely mechanical dispersion halos, which are defined as areas of distribution in the unconsolidated sediments of high amounts of minerals or indicator satellites. During the processes of physical weathering of the surface parts of the body of minerals occurring disintegration of the raw material, move wrecks as a result of the denudation in the lower parts of the relief, mechanical crushing them to release mineral concretions and a further full disclosure of the past to separate grains. At the same time in the forming of the material can be stored abrasive-resistant, low susceptible to mechanical wear minerals that have specific properties that determine the high hardness and density of these minerals, their low fragility and lack of cleavage. They are able to persist during transportation from indigenous sources and create so-called halo schlich mechanical type. Thus, schlich dispersion halos - halos is exogenous, provided the grains released by physico-chemically stable minerals, whose sizes range from a few millimeters to a few tenths of a millimeter. Distinct mechanical dispersion halos arise in the fields of native metals (gold, platinum group metals), diamonds, cassiterite, wolframite, ilmenite, rutile, zircon, monazite, and titanite, and searches are carried out schlich method. |