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.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.