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Devonian palaeogeography of the Southern Urals

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Treść / Zawartość
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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
Devonian deep-water deposits of the Southern Urals are represented mainly by flysch and cherty units. The main sedimentary basins (marginal sea and back-arc basin) and their origin, evolution and principal depositional environments are characterised. The main sources of clastic material were the Uraltau microcontinent (especially in the Famennian, when a mountain range formed following collision with an island arc) and two island arcs: the Irendyk, at the end of the Early and at the beginning of the Mid Devonian; and the Magnitogorsk, in the Mid to Late Devonian. Comparison with transgressive-regressive cycles established in Devonian epicontinental basins worldwide indicates that these global sea level fluctuations were recorded also in the Southern Urals deep-water settings. This applies primarily to the Eifelian and Frasnian-Famennian transgressive-regressive cycles.
Rocznik
Strony
205--216
Opis fizyczny
Bibliogr. 59 poz., rys., tab.
Twórcy
autor
  • Institute of Geology and Geochemistry, Urals Branch of the Russian Academy of Sciences, Pochtovy per., 7, RU-620151 Ekaterinburg, Russia, mizens@igg.uran.ru
Bibliografia
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Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BAT3-0016-0043
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