The paper “Early Cretaceous syn-rift uplift and tectonic inversion in the Loppa High area, southwestern Barents Sea, Norwegian shelf”, by Kjetil Indrevær, Roy Gabrielsen and Jan Inge Faleide, has been accepted for publishing by the Journal of Geological Society of London.

Abstract:

Tectonic inversion of rift basins is most commonly reported in the literature to occur after rifting has ceased. In contrast, we present evidence for syn-rift, localised tectonic inversion from the Loppa High area, southwestern Barents Sea and present a model for the formation of inversion structures as a result of differential uplift. The structures are of early Barremian to mid-Albian age (ca. 131-105Ma) and are focused in, or near pre-existing extensional boundary faults along the margins of the Loppa High. Inversion is interpreted to be the result of uplift of the high along its inclined boundary faults, leading to space accommodation problems as uplift was not properly compensated by extension in the region. The model constrains the initiation of uplift of the Loppa High to early Barremian and shows that the asymmetric margin configuration of the high may have led to a bulk clockwise rotation of the high around a vertical axis during uplift. The cause of uplift is not fully understood, but suggested to be linked to contemporaneous extreme lithospheric thinning in neighbouring basins to the west. Processes involved may include isostatic flexure, thermal heating, lithological phase changes and/or far-field stresses, although these aspects need to be further tested.

Reference:

Indrevær, K., Gabrielsen, Roy & Faleide, J.I. (in press): Early Cretaceous syn-rift uplift and tectonic inversion in the Loppa High area, southwestern Barents Sea, Norwegian shelf.  Accepted by Journal of the Geological Society of London. Doi: 10.1144/jgs2016-066 [intranet]