SLUMP STRUCTURES AS A TOOL TO RECOGNIZE SYNSEDIMENTARY FAULT ACTIVITY IN THE MIDDLE MEMBER OF THE BAKKEN FORMATION, WILLISTON BASIN, NORTH DAKOTA
The slumps reflect synsedimentary movements, e.g. along faults that were active during sedimentation. The study shows that the slumps follow known fault systems in the basin. Nevertheless, the net thickness of slumps allows for locating the structures more precisely as it is assumed that slumped units are thicker close to a fault. In order to assess fault activity, sequence stratigraphic surfaces such as parasequence boundaries are used to establish timelines within the middle Bakken member. Based on these timelines, the investigated fault systems show strongly varying amounts of synsedimentary activity: very active fault systems have slumps occurring throughout the succession. Other faults, in contrast, exhibit minor to no activity and are characterized by only a few slumps throughout the succession.
Areas accumulating slumps correspond to down-dip positions, or depositional troughs. The thickness of the middle Bakken member is, therefore, also a reflection of synsedimentary sediment movement, and the slump facies is limited to the downthrown side of the fault. Nevertheless, potential strike-slip faults do not show thickness variations mirroring uplifted and downthrown sides and may be exclusively detectable by such slumps. The presence of slumps shows that the middle Bakken member was characterized by high synsedimentary tectonic activity and therefore indicates that intracratonic basins are not as tectonically passive as previously thought.