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Pre-holocene joint fillings at Forsmark, Uppland, Sweden
Luleå University of Technology.
Geological Survey of Sweden, Sweden.
1975 (English)In: GFF, ISSN 1103-5897, E-ISSN 2000-0863, Vol. 97, no 1, p. 91-95Article in journal (Refereed) Published
Abstract [en]

Subhorizontal joints filled with sediments were found at Forsmark in north-eastern Uppland, Sweden. The sediments are glacial in character and show varves, graded and current bedding, and clay laminae. The occurrence, structure and pollen frequency of the sediments imply a deposition during a Pre-Holocene age, possibly during Early or Middle Weichsel.
Place, publisher, year, edition, pages
1975. Vol. 97, no 1, p. 91-95
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Geology
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URN: urn:nbn:se:ltu:diva-93882DOI: 10.1080/11035897509455477Scopus ID: 2-s2.0-84948049197OAI: oai:DiVA.org:ltu-93882DiVA, id: diva2:1709056
Available from: 2022-11-07 Created: 2022-11-07 Last updated: 2022-11-07Bibliographically approved

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