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Origin and significance of iron-oolitic sand-grains in the sediments of the Weser estuary

✍ Scribed by H. Lüneburg

Book ID
103257355
Publisher
Elsevier Science
Year
1964
Tongue
English
Weight
289 KB
Volume
1
Category
Article
ISSN
0025-3227

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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 ooids. The easternmost part of the oolite, from