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dc.contributor.authorCrowley, Peter D.
dc.coverage.spatialNARVIK
dc.coverage.spatial13312 Frostisen
dc.coverage.spatialHAMARØY
dc.date.accessioned2020-08-26T09:06:45Z
dc.date.available2020-08-26T09:06:45Z
dc.date.issued1989
dc.identifier.urihttps://hdl.handle.net/11250/2674182
dc.description.abstractThe Sitas area contains rock derived from the pre-Caledonian Scandinavian craton and from an accreted Caledonian fore-arc complex. These rocks form the par-authocthonous (?) Rombak Complex which can be tied stratigraphically to Baltica and three allochthons which from the base upwards are: the Storriten Complex, the Langvatn nappe and the Marko nappe. The Storriten Complex is a schuppen-zone composed of rocks derived from hinterland equivalents of the Rombak Complex while the Langvatn and Marko nappes are part of an accreted fore-arc terrane which can be correlated with parts of the Middle Køli Nappe Complex (MNKC). The Marko nappe contains mafic rocks whose geochemical affinites suggest derivation from both MORB-like and arc-like sources.
dc.language.isoeng
dc.relation.ispartofseriesNGU Bulletin (416)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectSTRUKTURGEOLOGI
dc.subjectTEKTONIKK
dc.subjectKALEDONSKE FJELLKJEDE
dc.subjectKARTLEGGING
dc.subjectOMDANNING
dc.titleThe Tectonostratigraphy and structural evolution of the Sitas Area, North Norway and Sweden (68°N).
dc.typeJournal article
dc.description.localcode35213
dc.source.pagenumber25-46


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