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Structure of the middle Urals, east of the Main Uralian Fault
Uppsala University.
Uppsala University.
1998 (English)In: GEOLOGICAL JOURNAL, ISSN 0072-1050, Vol. 33, no 1, 37-48 p.Article in journal (Other scientific) Published
Abstract [en]

In the Middle Urals, volcanic-are and back-are basin rocks of Ordovician to Devonian age occur in the Tagil Synform. These outboard terranes were thrust westwards in the late Carboniferous onto continental margin associations of late Proterozoic and Palae

Place, publisher, year, edition, pages
JOHN WILEY & SONS LTD , 1998. Vol. 33, no 1, 37-48 p.
Keyword [en]
Russia; Ural Mountains; metamorphic complexes; magmatic arcs; Palaeozoic; reflection seismology; SEISMIC-REFLECTION; CRUSTAL STRUCTURE; SOUTHERN URALS; EVOLUTION; MODEL; ROOT
Identifiers
URN: urn:nbn:se:uu:diva-28018OAI: oai:DiVA.org:uu-28018DiVA: diva2:55914
Note
Addresses: Friberg M, Uppsala Univ, Dept Geophys, Villavagen 16, S-75236 Uppsala, Sweden. Uppsala Univ, Dept Geophys, S-75236 Uppsala, Sweden. Urals Geol Mapping Expedit, UralGeolCom, Ekaterinburg, Sverdlovsk Dist, Russia.Available from: 2008-10-17 Created: 2008-10-17 Last updated: 2011-01-14

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