- 2017. Structural evolution of shearedmargin basins: the role of strain partitioning.Sørvestsnaget Basin, Norwegian Barents Sea. Basin Research. doi: 10.1111/bre.12253
- 2016. Depositional processes and stratigraphic architecture within a coarse-grained rift-margin turbidite system: The Wollaston Forland Group, east Greenland. Marine and Petroleum Geology. 76: 187-209. doi: 10.1016/j.marpetgeo.2016.05.018
- 2016. Structure and flow properties of syn-rift border faults: The interplay between fault damage and fault-related chemical alteration (Dombjerg Fault, Wollaston Forland, NE Greenland). Journal of Structural Geology. 92: 99-115. doi: 10.1016/j.jsg.2016.09.012
Reports and theses
- 2017. The structure and evolution of fault systems from outcrop to margin scale. Outcrop and subsurface insights from rift- and transtensional basins in East Greenland and the Western Barents Margin (offshore Norway). Universitetet i Bergen.
Fields of competence