title: Anomalous magnetization of the Permian-Triassic Nedubrovo red beds, Moscow basin
metadata.name: dc.contributor.author
metadata.value: Fetisova, Anna M.
metadata.lang: -
metadata.name: dc.contributor.author
metadata.value: Balabanov, Yuriy P.
metadata.lang: -
metadata.name: dc.contributor.author
metadata.value: Veselovskiy, Roman V.
metadata.lang: -
metadata.name: dc.contributor.author
metadata.value: Mamontov, Dmitriy A.
metadata.lang: -
metadata.name: dc.date.accessioned
metadata.value: 2019-04-01T16:28:31Z
metadata.lang: -
metadata.name: dc.date.available
metadata.value: 2019-04-01T16:28:31Z
metadata.lang: -
metadata.name: dc.date.issued
metadata.value: 2018-12
metadata.lang: -
metadata.name: dc.identifier.citation
metadata.value: Fetisova A. M., Balabanov Yu. P., Veselovskiy R. V., Mamontov D. A. Anomalous magnetization of the Permian-Triassic Nedubrovo red beds, Moscow basin. Vestnik of Saint Petersburg University. Earth Sciences, 2018, vol. 63, issue 4, pp. 544–560.
metadata.lang: en_GB
metadata.name: dc.identifier.other
metadata.value: 10.21638/spbu07.2018.409
metadata.lang: -
metadata.name: dc.identifier.uri
metadata.value: http://hdl.handle.net/11701/15422
metadata.lang: -
metadata.name: dc.description.abstract
metadata.value: A Nedubrovo member was recently described by (Lozovsky et al., 2001) and is the subject
  of continuing disputes due to the uncertainty of its age. Numerous determinations of fauna
  and flora allow to suggest the age of the Nedubrovo deposits as Upper Permian (Arefiev et
  al., 2016, Lozovsky et al., 2016) or Lower Triassic (Lozovsky et al., 2017). The uniqueness
  of the Nedubrovo member is also determined by the absence of its stratigraphic analogues
  within the Moscow sedimentary basin. Here we present the results of complex paleomagnetic
  and rock magnetic studies of the oldest Nedubrovo horizons of the Lower Triassic of the
  Moscow basin, which are outcropped in the lower stream of the Kichmenga River and lie on
  the clays of the Vyatkian stage of the Upper Permian. We found the paleomagnetic direction
  of the characteristic component of the magnetization of the studied red beds to be anomalous
  (slat = 60.04521°, slong = 45.74047°, N = 142, D = 246.3°, I = –6.6°, K = 10.0, α95 = 3.9°)
  and, with a high degree of probability, it corresponds to the period of significant and prolonged
  deviation of the Earth’s magnetic field configuration from the Geocentric Axial Dipole
  (GAD). The presence of anomalous paleomagnetic directions in Late Permian sedimentary
  and volcanic sections within Eurasia can be used as a powerful tool for local and regional
  magnetostratigraphic correlations, and it also indirectly suggests the Late Permian age of the
  Nedubrovo sediments.
metadata.lang: en_GB
metadata.name: dc.language.iso
metadata.value: ru
metadata.lang: en_GB
metadata.name: dc.publisher
metadata.value: St Petersburg State University
metadata.lang: en_GB
metadata.name: dc.relation.ispartofseries
metadata.value: Vestnik of St Petersburg University. Earth Sciences;Volume 63; Issue 4
metadata.lang: -
metadata.name: dc.subject
metadata.value: paleomagnetism
metadata.lang: en_GB
metadata.name: dc.subject
metadata.value: magnetostratigraphy
metadata.lang: en_GB
metadata.name: dc.subject
metadata.value: Permian-Triassic boundary
metadata.lang: en_GB
metadata.name: dc.subject
metadata.value: Russian sedimentary basin
metadata.lang: en_GB
metadata.name: dc.subject
metadata.value: Nedubrovo member
metadata.lang: en_GB
metadata.name: dc.title
metadata.value: Anomalous magnetization of the Permian-Triassic Nedubrovo red beds, Moscow basin
metadata.lang: en_GB
metadata.name: dc.type
metadata.value: Article
metadata.lang: en_GB
resources.filename: 09-Fetisova.pdf
resources.url: https://dspace.spbu.ru/bitstream/11701/15422/1/09-Fetisova.pdf
resources.format: Adobe PDF
resources.size: 5,76 MB