S4: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; whose development coincides; svalbard composite tectono; regional flooding surface; prominent provenance shift; oae1a ); separates; northerly source area; major flooding surface; kimmeridgian prograding shoreface; kapp toscana group; upper middle jurassic; dominated shelf deposits; middle jurassic; upper part; deltaic deposits; barents shelf; western spitsbergen; volcanism related; tse 6; thick organic; sill intrusions; sedimentary element; rich units; north caused; locally intersected; janusfjellet subgroup; helvetiafjellet formations; e .; deltaic wedges; deltaic system; central spitsbergen; carolinefjellet formation; barents sea; amerasian basin; Adventdalen; Arctic; Barents Sea; Carolinefjellet; Helvetiafjellet; Janusfjellet; Kapp Toscana; Rurikfjellet; Svalbard; Spitsbergen
• Online Access: https://doi.org/10.6084/m9.figshare.21968700.v1; https://figshare.com/articles/journal_contribution/S4_Svalbard_Composite_Tectono-Sedimentary_Element_Barents_Sea/21968700

The Middle Jurassic to Lower Cretaceous Adventdalen Group. TSE 6: Upper Middle Jurassic to Lower Cretaceous – continental platform. A prominent provenance shift to a northerly source area is recorded in the succession above the major flooding surface that caps the Kapp Toscana Group (Fig. a). The Ba...