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dc.contributor.authorWilson, J. Richard
dc.coverage.spatial16212 Selbu
dc.date.accessioned2020-07-15T07:40:50Z
dc.date.available2020-07-15T07:40:50Z
dc.date.issued2010
dc.identifier.issn0800-3416
dc.identifier.urihttps://hdl.handle.net/11250/2664628
dc.description.abstractThe Fongen-Hyllingen complex, situated 60 km southeast of Trondheim, Norway, comprises the 160 km2 Fongen-Hyllingen layered mafic intrusion (FH1) and the slightly younger, minor (3 km2) mafic to ultramafic Treknattan intrusion. The FH1 was emplaced synorogenically in the Scandinavian Caledonides -435 Ma ago. Folding and subsequent uplift and erosion allow access to the floor, walls and roof of the magma chamber. The complex itself has been affected to some extent by deformation and metamorphism, but sufficient primary features remain to study magma chamber processes in detail.
dc.language.isoeng
dc.relation.ispartofseriesNGU-Rapport (2010.015)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectBERGGRUNNSGEOLOGI
dc.subjectGABBRO
dc.subjectGANGBERGART
dc.subjectKALEDONSKE FJELLKJEDE
dc.subjectSTØRKNINGSBERGART
dc.titleThe Fongen - Hyllingen layered intrusion, Trondheim region, Norway: an excursion guide
dc.typeOthers
dc.description.localcode56432
dc.source.pagenumber146 s.
dc.relation.project(325100) Norges berggrunn - kartlegging og datasammenstilling


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