Issues of stratigraphy of the USSR
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Abstract
Geosynclinal and platform sedimentary complexes (formations)Geosynclinal sediments are intensely folded, metamorphosed and ruptured by synorogenic intrusions. They usually have a greater thickness - thousands of meters for a system and even for divisions of the system. Only in geosynclinal sediments are found flysch and molasse complexes, graywacke and aspid shale strata, and thick reef limestones.
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(Archived) Without section
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None
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