Genetic indices of halos surrounding ore mineralization are considered in the paper on the "ore body" hierarchical level. These indices have been correlated with the ore body ontogenesis (conception, growth, changes) and the three-membered structure of the zonal column: under-ore, the mere ore and over-ore parts. The differences between various types of metasomatites are displaied. A hypsometric nonconformity has been revealed between concentration maxima of analogous geochemical zones in the ore body and the surrounding halo. The movement of the concentration wave of an ore-forming element in allied zonal columns is described, as well as diagnostic signs of disseminated mineralization zones are indicated. The potential to carry out information from dissemination of minerals-indicators is shown by the example of pyrite. There is also a description of concentric alternating for zones of removement and concentration of siderophile elements which allows to trace the external boundary within the anomalous geochemical field hierarchy: ore body - field - ore deposit.
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