The New Siberian Islands and evidence for the continuation of the Uralides, Arctic Russia

• Main Authors: Pease, Victoria L., Kuzmichev, Alexander B., Danukalova, Maria K.
• Format: Dataset
• Language: unknown
• Published: Geological Society of London 2016
• Subjects: Geology; FOS Earth and related environmental sciences; Arctic; New Siberian Islands; Taimyr
• Online Access: https://dx.doi.org/10.6084/m9.figshare.3453830.v1; https://geolsoc.figshare.com/articles/dataset/The_New_Siberian_Islands_and_evidence_for_the_continuation_of_the_Uralides_Arctic_Russia/3453830/1

U–Pb detrital zircon results from New Siberian Islands sandstones illuminate the long-lived controversy regarding the continuation of the Uralian orogen into the Arctic region. A dominant age peak of c . 285 Ma from Permian sandstone requires proximal derivation from Taimyr’s Carboniferous–Permian granites, thought to reflect syn- to post-tectonic Uralian magmatism. The provenance of Devonian sandstone has Baltica affinities. The data record a dramatic change in provenance between Devonian and Permian time, from Baltica to a mixed Baltica + Uralian source. Our results confirm that the Uralian foreland basin extended from Taimyr to the New Siberian Islands.