Abstract
On the example of Nimansky gold-bearing region it was shown that the gold grains size depends on the depth of erosion dissection in case the original loads and climate conditions being of the same type within the metallogenic province. The largest grains are concentrated in those parts of river valleys, which are about 320-420 m in depth, the smallest ones - in the valleys about 160-240 m in depth. The valleys with the depth less then 120 m and more then 420 m have no commercial deposits.
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