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dc.contributor.authorBerthelsen, Asger
dc.coverage.spatial15324 Kirkesdalen
dc.coverage.spatial15321 Dividalen
dc.coverage.spatial15333 Takvatnet
dc.coverage.spatial15332 Tamokdalen
dc.date.accessioned2020-08-26T13:03:48Z
dc.date.available2020-08-26T13:03:48Z
dc.date.issued1967
dc.identifier.urihttps://hdl.handle.net/11250/2674859
dc.description.abstractThe geology and structures of two windows (the Mauken and the Divielva windows, see fig. 1) are outlined. For the Precambrian supracrustal rocks of the Mauken window, two formations names and one group name are suggested. Hyolithus zone sediments in autochthonous position along the southern margin of the Mauken window show that the Caledonian thrusting exeeded 70 km. In both window structures \"Relief\u00CFberschiebung\" took place. A magnetic anomaly in the Mauken window is explained by local concentrations of normally accessoric magnetite in an antiformal hinge zone in sericite-chlorite schists. The relations between an E-W directed magnetic anomaly and the structures of the Divielva window are discussed.
dc.language.isoeng
dc.relation.ispartofseriesNGU (247)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectGEOFYSIKK
dc.subjectPETROGRAFI
dc.subjectKARTLEGGING
dc.subjectPREKAMBRIUM
dc.subjectSTRUKTURGEOLOGI
dc.subjectANOMALI
dc.titleGeologic and structural studies around two geophysical anomalies in Troms, Northern Norway.
dc.typeJournal article
dc.description.localcode34904
dc.source.pagenumber57-77


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Navngivelse 4.0 Internasjonal
Except where otherwise noted, this item's license is described as Navngivelse 4.0 Internasjonal