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Active faults and paleoseismicity in Fennoscandia, especially Sweden. Primary structures and secondary effects
2004 (English)In: Tectonophysics, ISSN 0040-1951, E-ISSN 1879-3266, Vol. 380, no 3-4, 139-157 p.Article in journal (Refereed) Published
Abstract [en]

Fennoscandia, today a region of low to moderately low seismicity, was, at the time of deglaciation, with rates of uplift on the order of tens of centimetres per year, a region of very high seismicity and active tectonics. This is evident both from primary fault structures and from secondary sedimentary and hard rock effects in the region around the epicentral areas. The map of active faults in Fermoscandia includes numerous structures previously not recognised. Despite this, the recording of active faults and paleoseismic events is still in its initial phase. Much more data will surely accumulate in the near future. (C) 2004 Elsevier B.V. All rights reserved.

Place, publisher, year, edition, pages
2004. Vol. 380, no 3-4, 139-157 p.
Keyword [en]
deglaciation, faults, paleoseismicity
National Category
Geophysics
Identifiers
URN: urn:nbn:se:oru:diva-42444DOI: 10.1016/j.tecto.2003.09.018ISI: 000220257500004OAI: oai:DiVA.org:oru-42444DiVA: diva2:786503
Available from: 2015-02-05 Created: 2015-02-05 Last updated: 2015-02-05Bibliographically approved

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CiteExportLink to record
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