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Keywords Spitsbergen geology
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Abstract

An about 200-m long sandstone dyke cutting through the shales of the Janusfjellet Formation (Jurassic-Lower Cretaceous) has been discovered at Janusfjellet Central Spitsbergen. The palynomorph assemblage and the character of sandstone from the dyke are indicative of the Firkanten Formation of Paleocene age.

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Authors and Affiliations

Andrzej Wierzbowski
Maria Ziembińska-Tworzydło

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