Carboniferous graben structures, evaporite accumulations and tectonic inversion in the southeastern Norwegian Barents Sea

Author:

Hassaan Muhammad,Faleide Jan Inge,Gabrielsen Roy Helge,Tsikalas FilipposORCID

Funder

Research Council of Norway

Publisher

Elsevier BV

Subject

Stratigraphy,Economic Geology,Geology,Geophysics,Oceanography

Reference126 articles.

1. Polygonal mounds in the Barents Sea reveal sustained organic productivity towards the P–T boundary;Alves;Terra. Nova,2016

2. Paleozoic carbonates record the 4D evolution of salt domes in the Barents Sea;Alves,2019

3. Regional tectono-sedimentary development of the highs and basins of the northwestern Barents Shelf;Anell;Nor. Geol. Tidsskr.,2016

4. Cenozoic exhumation on the southwestern Barents Shelf: estimates and uncertainties constrained from compaction and thermal maturity analyses;Baig;Mar. Pet. Geol.,2016

5. Offshore prolongation of Caledonian structures and basement characterisation in the western Barents Sea from geophysical modelling;Barrère;Tectonophysics,2009

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