Replication Data for: Implications of Timanian thrust systems in the Barents Sea and Svalbard on using paleontological constraints for plate tectonics reconstructions

• Main Author: Koehl, Jean-Baptiste P.
• Other Authors: Koehl, Jean-Baptiste Philippe
• Format: Other/Unknown Material
• Language: unknown
• Published: DataverseNO 2023
• Subjects: Earth and Environmental Sciences; Paleontology; Tectonics; Trilobite; Biogeographical barrier; Fault; Fossil; Timanian; Caledonian; Svalbard; Barents Sea; Erosional unconformity; Faunal exchange; Plate tectonics; Neoproterozoic; Cambrian; Ordovician; Arctic; Arctic Ocean; Bjørnøya; Billefjorden; Hopen; Ny Friesland; Lomfjorden; Raddedalen; Plurdalen; Vimsodden; Bellsundbanken; Daudbjørnpynten; Kinnhøgda; Rijpdalen; Steiløya; Krylen; Kongsfjord*; Kongsfjorden; Storfjorden; Spitsbergen
• Online Access: https://doi.org/10.18710/BWZHL8

Figure_1a-b: high-resolution version of Figure 1a-b in the above-mentioned manuscript. Figure caption from the manuscript: (a) Overview of Timanian thrust systems and fingerprints in the Norwegian Arctic showing the location of the study area (white frame). The dashed black line marks the boundary between the Russian and Norwegian Barents Sea. (b) Overview of the study area in the Norwegian Barents Sea showing major Timanian thrust systems and the location of seismic profiles displayed in Figure 2. The basemap is the International Bathymetric Chart of the Arctic Ocean from Jakobsson et al. (2012). Abbreviations: AA: Atomfjella Antiform; BeFZ: Bellsundbanken fault zone; BFZ: Billefjorden Fault Zone; H2: Hopen-2 exploration well; KCFZ: Kongsfjorden–Cowanodden fault zone; KDFZ: Kinnhøgda–Daudbjørnpynten fault zone; LFZ: Lomfjorden Fault Zone; NY: Ny Friesland; P1: Plurdalen-1 exploration well; RA: Rijpdalen Anticline; R1: Raddedalen-1 exploration well; SKFZ: Steiløya–Krylen fault zone; Sø: Sørkapp; VKSZ: Vimsodden–Kosibapasset Shear Zone. Figure_2a: high-resolution version of Figure 2a in the above-mentioned manuscript. Figure caption from the manuscript: Seismic profiles (a) in Storfjorden, (b) south of Hopen, and (c) between Bjørnøya and Spitsbergen. The profiles show several kilometers thick, crustal-scale, dominantly NNE-dipping Timanian thrust systems (black lines) within Proterozoic basement rocks, and related overprints within lower Paleozoic, upper Paleozoic, and Mesozoic (–Cenozoic?) successions. The profiles also show major (erosional) unconformities between the Proterozoic basement, lower Paleozoic, and upper Paleozoic successions (white half-arrows). Figure_2b: high-resolution version of Figure 2b in the above-mentioned manuscript. Figure caption from the manuscript: Seismic profiles (a) in Storfjorden, (b) south of Hopen, and (c) between Bjørnøya and Spitsbergen. The profiles show several kilometers thick, crustal-scale, dominantly NNE-dipping Timanian thrust systems (black lines) within Proterozoic ...