Stochastic characteristics of sedimentation in evaporite basins: Potassium strata of Solikamsk deposit |
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Authors: | M. F. Mokhnach |
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Affiliation: | (1) Laboratory of Mathematical Geology, Steklov's Mathematical Institute, Academy of Sciences of the U.S.S.R., Leningrad, U.S.S.R. |
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Abstract: | The mode of alternation of halopelite, rock salt, and sylvinite beds in the Solikamsk deposit may be expressed in terms of Markov chains where each state is the lithologic composition of the bed. Both 2 and likelihood tests confirm the similarity of the Markov model with the actual geologic sections and suggest that evaporite sedimentation can be modeled by a renewal process. |
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Keywords: | Markov model halopelite rock salt sylvinite renewal process |
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