Structural Evolution at the Northeast North German Basin Margin: From Initial Triassic Salt Movement to Late Cretaceous‐Cenozoic Remobilization

dc.contributor.authorAhlrichs, Niklas
dc.contributor.authorHübscher, Christian
dc.contributor.authorNoack, Vera
dc.contributor.authorSchnabel, Michael
dc.contributor.authorDamm, Volkmar
dc.contributor.authorKrawczyk, Charlotte M.
dc.date.accessioned2020-11-10T14:58:36Z
dc.date.available2020-11-10T14:58:36Z
dc.date.issued2020-07-14
dc.date.updated2020-11-09T15:34:14Z
dc.description.abstractIn this study, we investigate the regional tectonic impact on salt movement at the northeastern margin of the intracontinental North German Basin. We discuss the evolution of salt pillows in the Bay of Mecklenburg in the light of thick‐ and thin‐skinned tectonics, including gravity gliding, and differential loading using seismic imaging. Stratigraphic and structural interpretation of a 170 km long, multichannel seismic line, extending from the Bay of Mecklenburg to northeast of Rügen Island, incorporates well information of nearby onshore wells. This new high‐resolution seismic line completely images the stratigraphic and tectonic pattern of the subsurface, from the base of the Zechstein to the seafloor. Our analysis reveals that subsidence during Late Triassic to Early Cretaceous at the northeastern basin margin was associated with transtensional dextral strike slip movement within the Trans‐European Suture Zone. We reinterpret the Werre and Prerow Fault Zones west of Rügen Island as an inverted, thin‐skinned normal fault system associated with the formation of the Western Pomeranian Fault System. Salt movement in the Bay of Mecklenburg was initiated in the Late Triassic and lasted until the Early Jurassic. A second phase of salt pillow growth occurred during the Coniacian until Cenozoic and correlates with compression‐related regional basin inversion due to the onset of the Africa‐Iberia‐Europe convergence. Thin‐skinned extensional initialization of salt pillow growth and compressional salt remobilization explains salt pillow evolution in the Bay of Mecklenburg. Additionally, we discuss an impact of gravity gliding on salt pillow evolution induced by basin margin tilt.en
dc.description.sponsorshipDFG, 61089689, SPP 1375: SAMPLE: South Atlantic Margin Processes and Links with onshore Evolutionen
dc.identifier.eissn1944-9194
dc.identifier.issn0278-7407
dc.identifier.urihttps://depositonce.tu-berlin.de/handle/11303/11888
dc.identifier.urihttp://dx.doi.org/10.14279/depositonce-10779
dc.language.isoenen
dc.rights.urihttps://creativecommons.org/licenses/by-nc/4.0/en
dc.subject.ddc550 Geowissenschaftende
dc.subject.otherMesozoic structural evolutionen
dc.subject.othersalt tectonicsen
dc.subject.otherBaltic Seaen
dc.subject.otherfaultsen
dc.subject.otherseismic imagingen
dc.subject.othergravity glidingen
dc.titleStructural Evolution at the Northeast North German Basin Margin: From Initial Triassic Salt Movement to Late Cretaceous‐Cenozoic Remobilizationen
dc.typeArticleen
dc.type.versionpublishedVersionen
dcterms.bibliographicCitation.articlenumbere2019TC005927en
dcterms.bibliographicCitation.doi10.1029/2019TC005927en
dcterms.bibliographicCitation.issue7en
dcterms.bibliographicCitation.journaltitleTectonicsen
dcterms.bibliographicCitation.originalpublishernameWileyen
dcterms.bibliographicCitation.originalpublisherplaceNew York, NYen
dcterms.bibliographicCitation.volume39en
tub.accessrights.dnbfreeen
tub.affiliationFak. 6 Planen Bauen Umwelt::Inst. Angewandte Geowissenschaften::FG Angewandte Geophysikde
tub.affiliation.facultyFak. 6 Planen Bauen Umweltde
tub.affiliation.groupFG Angewandte Geophysikde
tub.affiliation.instituteInst. Angewandte Geowissenschaftende
tub.publisher.universityorinstitutionTechnische Universität Berlinen

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