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dc.contributor.authorKnies, J.
dc.contributor.authorAndreassen, K.
dc.contributor.authorHusum, K.
dc.contributor.authorMattingsdal, R.
dc.contributor.authorFabian, K.
dc.contributor.authorGrøsfjeld, K.
dc.date.accessioned2020-07-15T07:30:31Z
dc.date.available2020-07-15T07:30:31Z
dc.date.issued2012
dc.identifier.issn0800-3416
dc.identifier.urihttps://hdl.handle.net/11250/2664529
dc.description.abstractOur major goal improving the chronostratigraphic framework for ODP site 910 and 911 from the marginal Arctic Ocean was successfully achieved. We have agreed on a new age model for both sites. We do not see any evidence for a hiatus in the sections. The collection of new high-resolution seismic data across the Yermak Plateau allows a perfect correlation between the sites. Both the new biostratigraphic and paleomagnetic data support the inferences from seismic correlation that the base of Hole 911A is slightly younger (~5.3 Ma) than Hole 910C (~5.8 Ma) (Fig. 1.1). The new data indicate that the base of the boreholes is approximately 2.5 Ma older than previously assigned (see ODP Leg 151 Scientific\/Initial Reports) (Fig. 1.2). All available old\/new age fixpoints for both boreholes are summarized in Table 1.1.
dc.language.isoeng
dc.relation.ispartofseriesNGU-Rapport (2012.034)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectSTRATIGRAFI
dc.subjectKRONOSTRATIGRAFI
dc.titleArctic chronology report
dc.typeReport
dc.description.localcode59801
dc.source.pagenumber43
dc.relation.project(327000) Arctic chronology project


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