Crustal structure and tectonic model of the Arctic region
O Petrov, A Morozov, S Shokalsky, S Kashubin… - Earth-Science …, 2016 - Elsevier
We present a new model of the crustal and tectonic structure of the Arctic region north of 60°
N latitude, constrained as a part of the international Atlas of Geological Maps of the …
N latitude, constrained as a part of the international Atlas of Geological Maps of the …
Structural inheritance in the North Atlantic
Abstract The North Atlantic, extending from the Charlie Gibbs Fracture Zone to the north
Norway-Greenland-Svalbard margins, is regarded as both a classic case of structural …
Norway-Greenland-Svalbard margins, is regarded as both a classic case of structural …
[HTML][HTML] EUNAseis: A seismic model for Moho and crustal structure in Europe, Greenland, and the North Atlantic region
IM Artemieva, H Thybo - Tectonophysics, 2013 - Elsevier
We present a new digital crustal model for Moho depth and crustal structure in Europe,
Greenland, Iceland, Svalbard, European Arctic shelf, and the North Atlantic Ocean (72W …
Greenland, Iceland, Svalbard, European Arctic shelf, and the North Atlantic Ocean (72W …
Crustal and basin evolution of the southwestern Barents Sea: From Caledonian orogeny to continental breakup
L Gernigon, M Brönner, D Roberts, O Olesen… - …, 2014 - Wiley Online Library
A new generation of aeromagnetic data documents the post‐Caledonide rift evolution of the
southwestern Barents Sea (SWBS) from the Norwegian mainland up to the continent‐ocean …
southwestern Barents Sea (SWBS) from the Norwegian mainland up to the continent‐ocean …
Circum-Arctic Lithosphere Evolution (CALE) Transect C: displacement of the Arctic Alaska–Chukotka microplate towards the Pacific during opening of the Amerasia …
This paper synthesizes the framework and geological evolution of the Arctic Alaska–
Chukotka microplate (AACM), from its origin as part of the continental platform fringing …
Chukotka microplate (AACM), from its origin as part of the continental platform fringing …
Quantification and restoration of the pre‐drift extension across the NE Atlantic conjugate margins during the mid‐Permian‐early Cenozoic multi‐rifting phases
The formation of the NE Atlantic conjugate margins is the result of multiple rifting phases
spanning from the Late Paleozoic and culminating in the early Eocene when breakup was …
spanning from the Late Paleozoic and culminating in the early Eocene when breakup was …
Tectonic implications of the lithospheric structure across the Barents and Kara shelves
This paper considers the lithospheric structure and evolution of the wider Barents–Kara Sea
region based on the compilation and integration of geophysical and geological data …
region based on the compilation and integration of geophysical and geological data …
Caledonian basement of the western Barents Sea
O Ritzmann, JI Faleide - Tectonics, 2007 - Wiley Online Library
Major crustal units in the western Barents Sea have been defined on the basis of depth‐
converted seismic reflection data, gravity and magnetic anomaly data. The seismic data …
converted seismic reflection data, gravity and magnetic anomaly data. The seismic data …
New insights into the tectono-stratigraphic evolution of the southern Stappen High and its transition to Bjørnøya Basin, SW Barents Sea
OA Blaich, F Tsikalas, JI Faleide - Marine and Petroleum Geology, 2017 - Elsevier
Within the context of the southwestern Barents Sea, the southern Stappen High and its
transition to the Bjørnøya Basin are still underexplored. Improved quality seismic reflection …
transition to the Bjørnøya Basin are still underexplored. Improved quality seismic reflection …
ArcCRUST: Arctic crustal thickness from 3‐D gravity inversion
N Lebedeva‐Ivanova, C Gaina… - Geochemistry …, 2019 - Wiley Online Library
The ArcCRUST model consists of crustal thickness and estimated crustal thinning factors
grids for the High Arctic and Circum‐Arctic regions (north of 67° N). This model is derived by …
grids for the High Arctic and Circum‐Arctic regions (north of 67° N). This model is derived by …