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Geological analysis illustrates the formation of neogenic deposits in southeastern Gorny Altai, suggesting tectonic influences.
Based on recent geological studies, the paleorelief of the bed of coaliferous Neogenic sediments is characterized, which is distinguished by moderate differentiation (100 to 450 m). Under analysis are ratios of long-lived faults in the rocks of pre-Paleozoic and Paleozoic basements to neogenetic post-Neogenic, with the former being renewed at the neotectonic stage. Essential features of the maintenance of coaliferous deposits and early stages of orogeny in the southeastern Gorny Altai are under discussion.
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Luzgin et al. (1992) studied this question.
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