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Below are the most common reasons: This site uses cookies to improve performance by remembering that you are logged in when you go from page to page.To provide access without cookies would require the site to create a new session for every page you visit, which slows the system down to an unacceptable level.Faculty of Geology, Moscow State University, Leninskie gory 1, Moscow RU-119991, Russia Abstract We present here a detailed study of the Upper Carboniferous–Lower Permian stratigraphy of Bol’shevik Island in the Severnaya Zemlya Archipelago, consisting of the analysis of sedimentary structures and lithostratigraphy, U/Pb detrital zircon dating and structural studies.

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It was hosted by Valuehost dedicated servers and colo subnet, Value Host Cloud Network and others.U/Pb dating of detrital zircons reveals that the Upper Carboniferous–Lower Permian sandstones contain a primary age population ranging from 450 to 570 millions of years, with a predominance of Early–Middle Ordovician zircons. This detrital zircon distribution indicates that the studied formations were derived locally from the erosion of Lower Ordovician deposits of Bol’shevik Island or elsewhere in the archipelago. E-mail: [email protected] access the supplementary material for this article, please see supplementary files under Article Tools online. If your browser does not accept cookies, you cannot view this site.

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