Abstract
During the Early Triassic, the lacustrine facies of the Moscow syneclise was regularly replaced eastward by alluvial-lacustrine and alluvial facies. The Early Triassic accumulation involved, in addition to the Moscow syneclise (its axial zone and northwestern slope), the Latvian saddle and the Polish-Lithuanian syneclise, that is, a sedimentation area significantly larger than the present one. Triassic sedimentation within the Moscow syneclise marked a new transgressive stage of the Hercynian tectogenic cycle and differed markedly from the Late Permian regressive stage of sedimentation. —Authors.
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