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Lomonosov Ridge: a double-sided continental margin
Ayred Wegener Institute for Polar and Marine Research.
Ayred Wegener Institute for Polar and Marine Research.
Ayred Wegener Institute for Polar and Marine Research.
Ayred Wegener Institute for Polar and Marine Research.ORCID iD: 0000-0002-1629-2920
1992 (English)In: Geology, ISSN 0091-7613, E-ISSN 1943-2682, Vol. 20, no 10, p. 887-890Article in journal (Refereed) Published
Abstract [en]

The first two traverses of marine multichannel seismic data across the Lomonosov Ridge (central Arctic), by the German research icebreaker Polarstern and the Swedish icebreaker Oden, demonstrate a prograded margin toward the Amerasian side and fault-bounded half grabens toward the Eurasian side of the ridge. Nearly 450m of undisturbed flat-lying strata have been deposited on top of the peneplaned ridge since it rifted from the Barents-Kara Sea margin and subsided below sea level in early Tertiary time (64-56 Ma) .

Place, publisher, year, edition, pages
1992. Vol. 20, no 10, p. 887-890
National Category
Geophysics
Research subject
Exploration Geophysics
Identifiers
URN: urn:nbn:se:ltu:diva-68837DOI: 10.1130/0091-7613(1992)020<0887:LRADSC>2.3.CO;2Scopus ID: 2-s2.0-84879885884OAI: oai:DiVA.org:ltu-68837DiVA, id: diva2:1209166
Available from: 2018-05-22 Created: 2018-05-22 Last updated: 2018-05-22Bibliographically approved

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