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A study of the earth's crust in the island area of Lofoten-Vesterålen, Northern Norway.

dc.contributor.authorSellevoll, Markvard
dc.coverage.spatial12324 Myre
dc.coverage.spatial10312 Flakstad
dc.coverage.spatial12333 Langenes
dc.coverage.spatial18301 Lofotodden
dc.coverage.spatialVESTVÅGØY
dc.coverage.spatialFLAKSTAD
dc.coverage.spatialMOSKENES
dc.date.accessioned2020-08-26T13:23:31Z
dc.date.available2020-08-26T13:23:31Z
dc.date.issued1983
dc.identifier.urihttps://hdl.handle.net/11250/2675158
dc.description.abstractThe present study is based on a reinterpretation of seismic refraction data as well as gravity data collected by the Seismological Observatory, University of Bergen in the island area of the Lofoten-Vesterålen, Northern Norway. The study shows a good agreement between the seismic and gravity modelling of the Moho depths along the profile line between the two shotpoints Hamnøy (Lofoten) and Stø (Vesterålen). A maximum Moho-depht of 26 km is observed about 85 km from Stø, and it would seem that the rse of the Moho towards Stø is moderate. On the other hand there is a distinct shallowing of the Moho beneath the Lofoten area.
dc.language.isoeng
dc.relation.ispartofseriesNGU (380)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectGEOFYSISK METODE
dc.subjectGRAVIMETRI
dc.subjectTOLKNING
dc.subjectMODELLFORSØK
dc.subjectREFLEKSJONSSEISMIKK
dc.titleA study of the earth's crust in the island area of Lofoten-Vesterålen, Northern Norway.
dc.typeJournal article
dc.description.localcode35463
dc.source.pagenumber235-243


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