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dc.contributor.authorCarstens, Harald
dc.coverage.spatial18131 Horten
dc.coverage.spatial15113 Kristiansand
dc.coverage.spatial18141 Asker
dc.coverage.spatial19164 Hamar
dc.coverage.spatialNESODDEN
dc.coverage.spatialKRISTIANSAND
dc.coverage.spatialRINGSAKER
dc.coverage.spatialVIKEN
dc.coverage.spatialAGDER
dc.coverage.spatialINNLANDET
dc.date.accessioned2020-08-26T12:54:30Z
dc.date.available2020-08-26T12:54:30Z
dc.date.issued1963
dc.identifier.urihttps://hdl.handle.net/11250/2674771
dc.description.abstractThe article presents detailed descriptions of the variolitic structure in selected minor intrusions and lavas. The evidence indicates that the varioles formed by liquid segregation rather than by spherulitic crystallization.
dc.language.isoeng
dc.relation.ispartofseriesNGU (223)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectMINERALOGI
dc.subjectSTØRKNINGSBERGART
dc.subjectKJEMISK ANALYSE
dc.subjectPERM
dc.subjectGANGBERGART
dc.subjectSTRUKTURGEOLOGI
dc.titleOn the variolitic structure.
dc.typeJournal article
dc.description.localcode35222
dc.source.pagenumber26-42


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    Artikler fra seriene NGU, NGU Bulletin og NGU Skrifter

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