S3:Svalbard Composite Tectono-Sedimentary Element, Barents Sea

• Main Authors: Snorre Olaussen, Sten-Andreas Grundvåg, Kim Senger, Ingrid Anell, Peter Betlem, Thomas Birchall, Alvar Braathen, Winfried Dallmann, Malte Jochmann, Erik P. Johannessen, Gareth Lord, Atle Mørk, Per T. Osmundsen, Aleksandra Smyrak-Sikora, Lars Stemmerik
• Format: Other Non-Article Part of Journal/Newspaper
• Language: unknown
• Published: 2023
• Subjects: Geology; svalbard composite tectono; paralic condensed deposits; kapp toscana groups; including zircon analysis; middle jurassic succession; barents sea triassic; middle jurassic; tse 5; southeastern part; southeast fennoscandia; shallow marine; sedimentary element; remaining part; prograding early; northwestward progradation; northeast greenland; giant delta; figs c; base triassic; Barents Sea; Greenland; Kapp Toscana; Sassendalen; Svalbard; Fennoscandia; Spitsbergen
• Online Access: https://doi.org/10.6084/m9.figshare.22007036.v1; https://figshare.com/articles/journal_contribution/S3_Svalbard_Composite_Tectono-Sedimentary_Element_Barents_Sea/22007036

Triassic to Middle Jurassic succession; Sassendalen and Kapp Toscana groups. TSE 5: Base Triassic to lower Middle Jurassic – sag basin. The northeastward- and eastward-prograding Early to early Middle Triassic coarser-grained shallow marine sandstones in the western Spitsbergen have petrography, including zircon analysis, affinity to basins on northeast Greenland (Fig. a). The remaining part of the Triassic was dominated by northwestward progradation of a giant delta with drainage from denudation of the Uralian and southeast Fennoscandia (Fig. b). Inversion and up-warping in latest Triassic–Early Jurassic on Spitsbergen was followed by shallow marine to paralic condensed deposits in the Middle Jurassic while the eastern and southeastern part of Svalbard experienced basin subsidence (Figs c and d).