Dividal-gruppen ("Hyolithus-sonen") i Finnmark og dens forhold til de eokambriske-kambriske formasjoner.

The stratigraphical members of the Dividal Group (also called the \"Hyolithus zone\") in Finnmark are compared with the Eocambrian-Cambrian sequence of the Tanafjrod-Laksefjord districts. The lower part of the Dividal Group falls within the Eocambrian while the upper part belongs to the Lo...

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Bibliographic Details
Main Author: Føyn, Sven
Format: Article in Journal/Newspaper
Language:Norwegian
Published: 1967
Subjects:
STRUKTURGEOLOGI
STRATIGRAFI
KALEDONSKE FJELLKJEDE
KARTLEGGING
PETROGRAFI
FOSSIL
Norway
Porsanger
Lebesby
Breivik
Skoganvarre
Finnmark
Lakselv
Northern Norway
Northern Sweden
Tana
Troms
Online Access:https://hdl.handle.net/11250/2674875
Description
Summary:The stratigraphical members of the Dividal Group (also called the \"Hyolithus zone\") in Finnmark are compared with the Eocambrian-Cambrian sequence of the Tanafjrod-Laksefjord districts. The lower part of the Dividal Group falls within the Eocambrian while the upper part belongs to the Lower Cambrian. The correctness of the correlation was confirmed by finds in 1966 of fragments of Platysolenites antiquissimus Eichw. in the Breivik Formation near the head of Laksefjord as well as in the \"member IV\" of the Dividal Group south of Porsangerfjord. Based on literature of the different members of the Dividal Group are traced along the south-eastern border of the Caledonian belt through Troms into northern Sweden, and a stratigraphical comparison is carried out between the areas at Tanafjord in northern Norway, Sjougd\u00E4lven in Sweden and Ringsaker in southern Norway. 34924

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