Extended data for "Caledonian reactivation and reworking of Timanian thrust systems and implications for latest Mesoproterozoic to mid-Paleozoic tectonics and magmatism in northern Baltica". The dataset includes the following: -Supplement 1: Overview of the (a) 2D and (b) 3D seismic reflection database uses in the present study. The maps also display the depth surfaces (in milliseconds TWT) of the main two Timanian thrusts mapped on the Finnmark Platform. -Supplement 2: (a–d) Uninterpreted seismic reflection data shown in Figure 2a–d. -Supplement 3: (a–d) Uninterpreted seismic reflection data shown in Figure 3a–d. -Supplement 4: (a–b) Uninterpreted seismic reflection data shown in Figure 4a–b. -Supplement 5: Resolution of 3D seismic survey FP13 and of 2D seismic survey BSS01. -Supplement 6: Zoom in bathymetric data in (a) the Nordkinn Peninsula, (b) west of the Nordkinn Peninsula in 3D with view towards the northeast, (c) the Repparfjord–Komagfjord tectonic window, (d) southeast of Rolvsøya, and (e) Sørøya. -Supplement 7: Zoom in interpreted and uninterpreted tilt derivative data from Nasuti et al. (2015) in (a) Magerøya, (b) Porsangerfjorden and the Sværholt Peninsula, (c) the Sværholt Peninsula and Nordkinn Peninsula, and (d) in Syltefjorden and Syltefjordfjellet. -Supplement 8: Zoom in interpreted and uninterpreted tilt derivative data from Nasuti et al. (2015) in (a) Sørøya, (b) Porsangerfjorden, the Sværholt Peninsula, and the Nordkinn Peninsula, and (c) the Digermulen Peninsula and the Varanger Peninsula. -Supplement 9: Interpreted (upper inset) and uninterpreted (lower inset) magnetic data from Gernigon et al. (2014) showing tens of kilometers wide anomalies interpreted as major folds.

Petrel, 2021.3

GlobalMapper, 13.0

CorelDraw, 2017