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Lower Ordovician iron ooids and associated oolitic clays in Russia and Estonia: a clue to the origin of iron oolites?
Uppsala University, Teknisk-naturvetenskapliga vetenskapsområdet, Earth Sciences, Department of Earth Sciences.
1999 (English)In: SEDIMENTARY GEOLOGY, ISSN 0037-0738, Vol. 123, no 1-2, 63-80 p.Article in journal (Refereed) Published
Abstract [en]

On the Baltic platform a lower Llanvirn (Ordovician) iron oolite can be traced for a distance of 1200 km from Norway to the east of Lake Ladoga in Russia. This oolite is usually thin (seldom exceeding 0.5 m) and is dominated by goethite (limonite) type oo

Place, publisher, year, edition, pages
ELSEVIER SCIENCE BV , 1999. Vol. 123, no 1-2, 63-80 p.
Keyword [en]
Ordovician; iron ooid; Russia; Estonia; volcanism; isotope; neodymium; REE; K-BENTONITES; VOLCANIC ASH; DISCRIMINATION; MOBILITY; ELEMENTS; SWEDEN; SR; ND
URN: urn:nbn:se:uu:diva-27774OAI: oai:DiVA.org:uu-27774DiVA: diva2:55670
Addresses: Sturesson U, Uppsala Univ, Inst Earth Sci, Norbyvagen 22, S-75236 Uppsala, Sweden. Uppsala Univ, Inst Earth Sci, S-75236 Uppsala, Sweden.Available from: 2008-10-17 Created: 2008-10-17 Last updated: 2011-01-14

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