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dc.contributor.authorBartley, John M.
dc.coverage.spatial12322 Gullesfjorden
dc.coverage.spatial12321 Kvæfjord
dc.coverage.spatial13324 Harstad
dc.coverage.spatial13323 Tjeldsundet
dc.coverage.spatialTROMS OG FINNMARK
dc.coverage.spatialKVÆFJORD
dc.coverage.spatialHARSTAD
dc.coverage.spatialNORDLAND
dc.coverage.spatialTJELDSUND
dc.date.accessioned2020-08-26T13:21:21Z
dc.date.available2020-08-26T13:21:21Z
dc.date.issued1981
dc.identifier.urihttps://hdl.handle.net/11250/2675123
dc.description.abstractThe Storvann Group is a sequence of metasedimentary rocks which constitutes the autochtohonous Cambrian (?) sedimentary cover of the Precambrian Lofoten terrane on east Hinnøy, North Norway. The Storvann Group is composed of impure quartzite overlain by progressively more aluminous quartz-rich schists, with subordinate calcite marbles, comprising a transgressive sequence. The general stratigraphic similarity of the Storvann Group to autochthonous, unmetamorphosed sedimentary rocks of the Scandinavian platform supports a recent hypothesis that the Lofoten terrane was part of the Baltoscandian continental block prior to Caledonian orogenesis. The composition of the Storvann Group suggests a platformal or miogeoclinal environment of deposition. However, without some means of determining the original thickness and stratigraphic continuity of this sequence, the position it represents relative to the pre-Caledonian Baltoscandian continental edge remains unknown.
dc.language.isoeng
dc.relation.ispartofseriesNGU (370)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectLITOSTRATIGRAFI
dc.subjectSEDIMENTÆR BERGART
dc.subjectSTRANDFORSKYVNING
dc.titleLithostratigraphy of the Storvann Group, east Hinnøy, North Norway, and its regional implications.
dc.typeJournal article
dc.description.localcode36056
dc.source.pagenumber11-24


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