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dc.contributor.authorHansen, Martin Bak
dc.date.accessioned2010-10-12T19:28:33Z
dc.date.available2010-10-12T19:28:33Z
dc.date.issued2007
dc.identifier.urihttp://hdl.handle.net/11858/00-1735-0000-0001-31B7-6
dc.description.abstractDuring several marine geophysical data acquisition cruises in the western Baltic Sea, for the Baltseis and NeoBaltic projects, a dense grid of 2D high-resolution multichannel seismics and to some extend gravity and magnetic data were acquired in the German and Danish territorial waters of the region. The western Baltic Sea comprises the northern part of the Northeast German Basin on the southern flank of the Ringkøbing-Fyn High. Furthermore, parts of the suture zone between the Avalonia and Baltica plates (the Caledonian Deformation Front) and the Sorgenfrei Tornquist Zone were investigated during these research cruises. Adjacent to the study area two structures are located, which are important for the structural evolution in the region. To the west the N-S trending Glückstadt Graben and in the eastern part the E-W running Grimmen High...
dc.format.mimetypeapplication/pdf
dc.language.isoeng
dc.publisherUniv. Hamburg
dc.rights.urihttp://e-docs.geo-leo.de/rights
dc.subject.ddc550
dc.subject.gokVBM 000
dc.subject.gokVAE 820
dc.subject.gokTSB 000
dc.subject.gokVEB 110
dc.subject.gokTQC 200
dc.titleStructure and evolution of the northern part of the Northeast German Basin revealed from seismic interpretation and 3D structural modelling
dc.typemonograph
dc.subject.gokverbalGeologische Interpretation geophysikalischer Beobachtungen
dc.subject.gokverbalSedimentationsbecken als Erdkrustentypen {Geologie}
dc.subject.gokverbalMitteleuropa {Geophysik}
dc.subject.gokverbalNorddeutsche Senke {Geologie}
dc.subject.gokverbalProspektionsseismik {Geophysik}
dc.identifier.doi10.23689/fidgeo-300
dc.identifier.ppn573775982
dc.identifier.urnurn:nbn:de:gbv:18-31578
dc.type.versionpublishedVersion
dc.relation.collectionGeophysik
dc.description.typethesis


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