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This article explores the composition and structure of stormogenic limestone deposits in the Siberian Platform, suggesting their significance for event stratification.
The article deals with specific features of the composition and the structure of heteroblastic limestones forming tabular bodies among monotonously laminated limestone-marl depositions of the Middle-Upper Cambrian in the northern Siberian Platform. They are proven to belong to stormogenic formations and to be of great importance for the event stratification.
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M. A. Minaeva (1992) studied this question.
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