On Ammonites from Spitsbergen
- 1 August 1921
- journal article
- research article
- Published by Cambridge University Press (CUP) in Geological Magazine
- Vol. 58 (8) , 347-356
- https://doi.org/10.1017/s0016756800104662
Abstract
There appears to be a good deal of variation in the Lower Triassic succession of the different parts of Spitsbergen, even between Ice Fjord and Bell Sound, at which latter Gyronites nathorsti J. Böhm occurs in soft shales. The grey sandstones with a Lamellibranch fauna of Werfenian age from Axel Island, again, represent quite a different facies.Keywords
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