title: Carboniferous Granitoid Magmatism of Northern Taimyr: Results of Isotopic-Geochemical Study and Geodynamic Interpretation
metadata.name: dc.contributor.author
metadata.value: Худолей, Андрей Константинович
metadata.lang: -
metadata.name: dc.date.accessioned
metadata.value: 2020-09-08T16:01:28Z
metadata.lang: -
metadata.name: dc.date.available
metadata.value: 2020-09-08T16:01:28Z
metadata.lang: -
metadata.name: dc.date.issued
metadata.value: 2018
metadata.lang: -
metadata.name: dc.identifier.uri
metadata.value: http://hdl.handle.net/11701/19270
metadata.lang: -
metadata.name: dc.description.abstract
metadata.value: Data on the petrography, geochemistry, and isotopic geochronology of granites from the northern
  part of the Taimyr Peninsula are considered. The Early–Middle Carboniferous age of these rocks has been
  established (U–Pb, SIMS). Judging by the results of 40Ar/39Ar dating, the rocks underwent metamorphism in
  the Middle Permian. In geochemical and isotopic composition, the granitic rocks have much in common with
  evolved I-type granites. This makes it possible to specify a suprasubduction marginal continental formation setting.
  The existence of an active Carboniferous margin along the southern edge of the Kara Block (in presentday
  coordinates) corroborates the close relationship of the studied region with the continent of Baltia.
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: Carboniferous Granitoid Magmatism of Northern Taimyr: Results of Isotopic-Geochemical Study and Geodynamic Interpretation
metadata.lang: en_GB
metadata.name: dc.type
metadata.value: Article
metadata.lang: en_GB
resources.filename: Kurapov-et-al-2018-Gt.pdf
resources.url: https://dspace.spbu.ru/bitstream/11701/19270/1/Kurapov-et-al-2018-Gt.pdf
resources.format: Adobe PDF
resources.size: 1,82 MB