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The late Neoproterozoic Enganepe ophiolite, Polar Urals, Russia: An extension of the Cadomian arc?
Uppsala University, Teknisk-naturvetenskapliga vetenskapsområdet, Earth Sciences, Department of Earth Sciences.
2001 (English)In: PRECAMBRIAN RESEARCH, ISSN 0301-9268, Vol. 110, no 1-4, p. 255-275Article in journal (Refereed) Published
Abstract [en]

The Enganepe ophiolite, Polar Urals was formed at similar to 670 Ma and records a diverse geochemical association of tholeiite, arc-tholeiite, adakite, and GIB-like lithologies. This constrains the tectonic setting of the protolith of the ophiolite to an

Place, publisher, year, edition, pages
ELSEVIER SCIENCE BV , 2001. Vol. 110, no 1-4, p. 255-275
Keyword [en]
Arc-continent collision; cadomian arc; geochemistry; ophiolite; Polar Urals; Rodinia; YOUNG OCEANIC LITHOSPHERE; ISLAND-ARC; VOLCANIC-ROCKS; SM-ND; MANTLE STRUCTURE; DACITE GENESIS; CRUSTAL GROWTH; SOUTHERN URALS; UNITED-STATES; SLAB
Identifiers
URN: urn:nbn:se:uu:diva-37874OAI: oai:DiVA.org:uu-37874DiVA, id: diva2:65773
Note
Addresses: Scarrow JH, Univ Granada, Dept Mineral & Petrol, Campus Fuentenueva, Granada 18002, Spain. Univ Udine, Dept Georisorse & Terr, I-33100 Udine, Italy. Univ Uppsala, Dept Earth Sci, SE-75236 Uppsala, Sweden. Univ Rennes 1, CNRS, Upr 4661, Bur 122,Available from: 2008-10-17 Created: 2008-10-17 Last updated: 2011-01-14

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