Abstract
Problems of the origin and tectonic pattern of the South Verkhoyansk sinclinorium are discussed. It is suggested that in the Late Paleozoic the South Verkhoyansk basin inherited the structure of the Sette-Daban rift graben and, as a submarine valley, was positioned across the Vtrkhoyansk passive margin. Lateral motions of the Okhotsk indentor in course of Late Mesozoic orogenic events led to transformation of the South Verkhoyansk basin into the same name two-stade sinclinorium of which the lower cleavage stage represents as ore-bearing metamorphic layer.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: 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.
