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Bates, D. E. B., Schwarzacher, W. (1958) The Geology of the Land between Ekmanfjorden and Dicksonfjorden in Central Vestspitsbergen. Geological Magazine, 95 (3) 219-233 doi:10.1017/s0016756800066139

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Reference TypeJournal (article/letter/editorial)
TitleThe Geology of the Land between Ekmanfjorden and Dicksonfjorden in Central Vestspitsbergen
JournalGeological Magazine
AuthorsBates, D. E. B.Author
Schwarzacher, W.Author
Year1958 (June)Volume95
Issue3
PublisherCambridge University Press (CUP)
DOIdoi:10.1017/s0016756800066139
Generate Citation Formats
Mindat Ref. ID248776Long-form Identifiermindat:1:5:248776:6
GUID0
Full ReferenceBates, D. E. B., Schwarzacher, W. (1958) The Geology of the Land between Ekmanfjorden and Dicksonfjorden in Central Vestspitsbergen. Geological Magazine, 95 (3) 219-233 doi:10.1017/s0016756800066139
Plain TextBates, D. E. B., Schwarzacher, W. (1958) The Geology of the Land between Ekmanfjorden and Dicksonfjorden in Central Vestspitsbergen. Geological Magazine, 95 (3) 219-233 doi:10.1017/s0016756800066139
In(1958, June) Geological Magazine Vol. 95 (3) Cambridge University Press (CUP)
Abstract/NotesAbstractThe peninsula between Ekmanfjorden and Dicksonfjorden has been mapped geologically. Devonian sandstones are overlain unconformably by a Permo-Carboniferous sequence of limestones (200 m.) and dolomites and gypsum (300 m.). This is followed by more than 150 metres of Permian cherts. The strata show a slight but consistent dip towards the SSE. A fault having the trend of this dip has been proved in Ekmanfjorden. Sills are intruded in the higher levels of the succession and it is suggested that the intrusions are contemporaneous with the faulting. By comparing the lithology the area can be correlated with the known sections of Billefjorden and Kongsfjorden.


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