Abstract
The paper considers the conditions of formation of novokrivorozhskaya suite that meets the basis of the section of Kryvyi Rih structure. Paleogeographic reconstructions novokrivorozhskaya suite was based on these methods: comparison of intensity factors of weathering and sedimentary differentiation of A.A. Predovsky, the attitude indicator elements and depositional facies conditions – the conditions of sedimentation. Using techniques of V.K. Golovenok, and by comparing the chemical composition of rocks novokrivorozhskaya suite with an average composition of rock-forming oxides clarke in magmatic rocks there was the attempt to reconstruct the climatic conditions of sedimentation suite. The formation analysis usage allowed to determine the likely sources of clastic material and ways of transportation.
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