title: U–Pb LA–ICP–MS Age of Detrital Zircons from the Lower Riphean and Upper Vendian Deposits of the Luga–Ladoga Monocline
metadata.name: dc.contributor.author
metadata.value: Худолей, Андрей Константинович
metadata.lang: -
metadata.name: dc.date.accessioned
metadata.value: 2020-09-08T15:52:12Z
metadata.lang: -
metadata.name: dc.date.available
metadata.value: 2020-09-08T15:52:12Z
metadata.lang: -
metadata.name: dc.date.issued
metadata.value: 2018
metadata.lang: -
metadata.name: dc.identifier.uri
metadata.value: http://hdl.handle.net/11701/19266
metadata.lang: -
metadata.name: dc.description.abstract
metadata.value: The results of LA–ICP–MS U–Pb analyses of detrital zircons from the Precambrian deposits of
  Luga–Ladoga monocline are discussed. The age spectra of the zircons separated from the Riphean to Upper
  Vendian sandstones from the Shotkusa-1 well demonstrate dominance of the Paleo- and Mesoproterozoic
  grains while the Archaean zircons are subordinate. The Riphean debris sources were local swells of the Northern
  Ladoga basement. The sequence interval presumably corresponding to the Vasilieostrov Formation
  (Upper Vendian) has yielded not only Paleo- and Mesoproterozoic zircon ages, but Neoproterozoic as well,
  implying a Timanide provenance: these zircons (527 ± 9 and 516 ± 13 Ma) allow deposition of a significant
  part of the Shotkusa-1 sequence at the very beginning of the Cambrian.
metadata.lang: en_GB
metadata.name: dc.language.iso
metadata.value: en
metadata.lang: en_GB
metadata.name: dc.publisher
metadata.value: Pleiades Publishing, Ltd
metadata.lang: en_GB
metadata.name: dc.title
metadata.value: U–Pb LA–ICP–MS Age of Detrital Zircons from the Lower Riphean and Upper Vendian Deposits of the Luga–Ladoga Monocline
metadata.lang: en_GB
metadata.name: dc.type
metadata.value: Article
metadata.lang: en_GB
resources.filename: Ivleva-et-al-2018-DAN.pdf
resources.url: https://dspace.spbu.ru/bitstream/11701/19266/1/Ivleva-et-al-2018-DAN.pdf
resources.format: Adobe PDF
resources.size: 759,72 kB