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Intercommunication between plicate and break violations of coal layers (on example of field of mine “Krasnodarskaya-Yuzhnaya”)

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Category: Geological sciences

Last Updated on Wednesday, 28 November 2012 13:42

Published on Wednesday, 21 November 2012 15:48

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Authors: 

V.F. Prikhodchenko, Doctor of Geological Science, Professor, State Higher Educational Institution “National Mining University”, Head of the Department of Geology and Survey of Mineral Deposits, Dnipropetrovsk, Ukraine

S.I. Shabelnikov, Donbass State Technical University, Assistant Lecturer of the Department of Surveying, Geology and Geodesy, Alchevsk, Ukraine

D.V. Tolubets, State Higher Educational Institution “National Mining University”, Assistant Lecturer of the Department of Geology and Survey of Mineral Deposits, Dnipropetrovsk, Ukraine

Annotation:

On the example of mine “Krasnodarskaya-Yuzhnaya”, located on the territory of Krasnodon coal-bearing area, patterns of variability of small-amplitude disjunctive breaks of the coal beds, depending on the width and amplitude of the compressive disturbances coal-bearing strata are shown. According to the data from mine workings changes in the number of disjunctive dislocations formed during the formation of folded structures, is subject to a polynomial dependence.

References:

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