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We present results of a multidisciplinary study of the northern segment of the Vøring volcanic rifted margin, offshore mid‐Norway. This segment represents a transitional margin domain that is less investigated compared to the adjacent segments of the margin. In order to understand the geological evolution of the study area, we performed an integrated interpretation of an extensive geological and geophysical data set. This data set includes recently acquired and reprocessed 2‐D reflection seismic, published refraction data and potential field data, as well as new borehole data. Two‐dimensional potential field modeling was performed to better assess the crustal architecture and evolution of the northern Vøring Margin. We then consider how crustal‐scale structures and processes affected the basin formation. The outer and distal northern Vøring Margin represents a series of deep Cretaceous (Træna Basin and Någrind Syncline) and Cretaceous‐Paleocene (Hel Graben) sag subbasins underlain by a significantly thinned continental crust. These subbasins developed in between structural highs (Utgard, Nyk, and Grimm Highs), which are underlain by a thicker crust and interpreted as a series of rigid continental blocks (“buffers”). In addition to the regional Late Jurassic‐Early Cretaceous rifting events, we found structural evidence of local Neocomian and mid‐Cretaceous extensional reactivation affecting the northern segment of the Vøring Basin. During the mid‐Late Cretaceous‐Paleocene, the extensional axis within the Vøring Basin province migrated sequentially northwestward to the present‐day continent‐ocean “boundary”. We also show fundamental differences between the volcanic rifted mid‐Norwegian Margin and nonvolcanic (Iberian‐type) margins and how preexisting structures events can shape the evolution and architecture of the margin.

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