The influence of halokinesis on prograding clinoforms: Insights from the Tiddlybanken Basin, Norwegian Barents Sea

• Published in: Basin Research
• Main Authors: Rojo, Luis Alberto, Marín, Dora, Cardozo, Nestor, Escalona, Alejandro, Koyi, Hemin
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2019
• Subjects: Barents Sea
• Online Access: http://dx.doi.org/10.1111/bre.12411; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fbre.12411; https://onlinelibrary.wiley.com/doi/pdf/10.1111/bre.12411; https://onlinelibrary.wiley.com/doi/full-xml/10.1111/bre.12411

Abstract Although the trajectory and geometry of clinoforms in different types of basins have been described in many studies, few studies discuss the influence of halokinesis on clinoforms in salt‐related basins. In this study, we analyse the Lower Cretaceous clinoforms in the Tiddlybanken Basin, Norwegian Barents Sea to evaluate the impact of salt mobilization on the geometry and trajectory of clinoforms as well as its implications on sediment partitioning. To accomplish this objective, we use a multidisciplinary approach consisting of seismic and well‐interpretation, 3D structural restoration, and forward stratigraphic modelling. The results show that salt mobilization affects prograding clinoforms by: (a) causing lateral variations in progradation rates, resulting in complex palaeogeography, (b) increasing slope angles, which affect the equilibrium of the clinoform profile and can trigger slope‐readjustment processes and (c) producing lateral and temporal variations in accommodation space, leading to different clinoform trajectories, stacking patterns and reservoir distribution along the basin. Forward stratigraphic modelling shows that in salt‐related basins and other tectonically active basins, the isolated use of conventional methods for clinoform analysis might lead to potential interpretation pitfalls such as misinterpretation of trajectories and overestimation of foreset angles, which can have negative consequences for exploration models.