title: Folded structures of the southeastern and western vergency of the Maksyutov metamorphic complex of the Southern Urals
metadata.name: dc.contributor.author
metadata.value: Golionko, Boris G.
metadata.lang: -
metadata.name: dc.contributor.author
metadata.value: Ryazantsev, Alexey V.
metadata.lang: -
metadata.name: dc.date.accessioned
metadata.value: 2020-12-17T10:52:48Z
metadata.lang: -
metadata.name: dc.date.available
metadata.value: 2020-12-17T10:52:48Z
metadata.lang: -
metadata.name: dc.date.issued
metadata.value: 2020-09
metadata.lang: -
metadata.name: dc.identifier.citation
metadata.value: Golionko B.G., Ryazantsev A.V. (2020). Folded structures of the southeastern and western vergency of the Maksyutov metamorphic complex of the Southern Urals. Vestnik of Saint Petersburg University. Earth Sciences, 65 (3), 506–527.
metadata.lang: en_GB
metadata.name: dc.identifier.other
metadata.value: https://doi.org/10.21638/spbu07.2020.306
metadata.lang: -
metadata.name: dc.identifier.uri
metadata.value: http://hdl.handle.net/11701/21692
metadata.lang: -
metadata.name: dc.description.abstract
metadata.value: The structural evolution of the Maksyutov metamorphic complex in the southern part of the
  Uraltau zone (Southern Urals) was investigated. Several stages of deformation were distinguished. The first stage of deformation is associated with the formation of F1 folds, which include folded structures of the southwestern vergence and sheath folds. The second stage was
  expressed in the formation of F2 folds of the southeastern vergence, the most common in the
  field of development of the Maksyutov metamorphic complex. An alternative model involves the
  formation of sheath folds as the main structures and folds of the southwestern and southeastern
  vergence as additional ones under the conditions of tectonic movements in the direction from
  NE to SW.The choice between the two models requires additional research. The early stages of
  the deformation history of the complex are associated with the exhumation of its rocks from the subduction zone of the Magnitogorsk island arc. The next stage was expressed in the formation
  of F3 folds of the western vergence associated with movements along the Main Ural Fault zone,
  during the Late Paleozoic collision. Post-collision shear movements marked by F4 folds with
  steeply dipping hinges completed the main stage of the region’s structural evolution.
metadata.lang: en_GB
metadata.name: dc.description.sponsorship
metadata.value: The research was carried out within the state assignment 0135-2016-0009 and supported by the
  Russian Foundation for Basic Research (project no. 20-05-00308).
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 65; Issue 3
metadata.lang: -
metadata.name: dc.subject
metadata.value: Uraltau zone
metadata.lang: en_GB
metadata.name: dc.subject
metadata.value: structural evolution
metadata.lang: en_GB
metadata.name: dc.subject
metadata.value: deformation stage
metadata.lang: en_GB
metadata.name: dc.subject
metadata.value: asymmetric folds
metadata.lang: en_GB
metadata.name: dc.subject
metadata.value: sheath folds
metadata.lang: en_GB
metadata.name: dc.subject
metadata.value: hinge
metadata.lang: en_GB
metadata.name: dc.subject
metadata.value: lineation
metadata.lang: en_GB
metadata.name: dc.subject
metadata.value: Maksyutov metamorphic complex
metadata.lang: en_GB
metadata.name: dc.subject
metadata.value: vergence
metadata.lang: en_GB
metadata.name: dc.title
metadata.value: Folded structures of the southeastern and western vergency of the Maksyutov metamorphic complex of the Southern Urals
metadata.lang: en_GB
metadata.name: dc.type
metadata.value: Article
metadata.lang: en_GB
resources.filename: 506-527.pdf
resources.url: https://dspace.spbu.ru/bitstream/11701/21692/1/506-527.pdf
resources.format: Adobe PDF
resources.size: 10,41 MB