Srpukhovskian Stage of the western part of the Zaisan fold system
Abstract
In most areas of W. Kazakhstan, the boundary between the Lower and Middle Carboniferous is indistinct, gradual, which is the reason for the allocation of local stratigraphic subdivisions, the age of which is interpreted as Upper Namur-Middle Carboniferous undissected or as Upper Namur-Middle Carboniferous ...
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(Archived) Without section
References
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