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- W2016069409 abstract "Spitsbergen (Svalbard) is traversed by several major fault systems trending approximately N-S. One of them, the Billefjorden Fault Zone (BFZ), is a major long-lived lineament on Spitsbergen (Harland et al., 1974; Birkenmajer, 1975) running the length of Wijdefjorden in N Spitsbergen. The BFZ has been interpreted to be part of a major Late Devonian transform fault, and more than 200 km sinistral strike-slip movement has been suggested (Harland et al., 1974). The BFZ is well exposed for only 80 km north of Billefjorden, and is buried beneath the sedimentary cover in S Spitsbergen. It is therefore not known if the BFZ extends to the south of Spitsbergen into the barents Sea." @default.
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- W2016069409 date "1993-01-01" @default.
- W2016069409 modified "2023-09-25" @default.
- W2016069409 title "A Study of geophysical data from the Billefjorden Fault Zone, Spitsbergen (Svalbard)" @default.
- W2016069409 doi "https://doi.org/10.3997/2214-4609.201411473" @default.
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