
The results of our research suggest that Lower Cretaceous, coarse-grained wedges in the southwestern Barents Sea (and Norwegian Sea) are point- and linear- sourced, either banked to basin margins and internal basin highs or terraces close to master faults.
In addition, two main progradational margins, sourced from large continental land areas to the W-NW and E-NE, may have provided coarse-grained sediments to basinal areas in the southwestern Barents Sea.
Therefore, specific evidences of the ...
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