No abstract

Fractured carbonate rocks are widely used as hydrocarbon or geothermal reservoirs.To provide a better understanding of the distribution and characteristics of such fractures, a general workflow will be presented for the characterization of fracturing from borehole data, by exploration and statistical analyses of integrated datasets. In a case study of Viséan limestones in a Belgian borehole, both cores and geophysical well logs were used to investigate which factors control the characteristics of partially open veins, which contribute to permeability. Relationships between multiple variables were tested statistically. Lithology, geochemistry and geophysical well log values were taken into account, as well as quantified veins, vugs and stylolites from cores. Although natural joint frequencies appeared hard to quantify from the available data, partially open vein characteristics could be well quantified. The results show that differential compaction controlled the development of fractures. Fracturing occurred preferentially in massive reefal buildup boundstones in contrast to layered wacke-to grainstones. Layer-parallel slip along bedding surfaces could also have reduced fracture development in the latter limestones. Frequencies of cemented veins and partially open veins are positively correlated, which suggests that the partially open veins result from either re-opening by dissolution, or (re-)opening due to a later fracturation phase. In summary, this multi-source study provides a workflow for fracture characterization from boreholes, as well as insights into the factors controlling the distribution and characteristics of partially open veins, which enhance reservoir permeability.

In contrast to the Norwegian and Danish sectors, where significant hydrocarbon reserves were found in chalk reservoirs, limited studies exist analysing the chalk evolution in the Dutch part of the North Sea. To provide a better understanding of this evolution, a tectono-sedimentary study of the Late Cretaceous to Early Palaeogene Chalk Group in the northern Dutch North Sea was performed, facilitated by a relatively new 3D seismic survey. Integrating seismic and biostratigraphic well data, seven chronostratigraphic units were mapped, allowing a reconstruction of intra-chalk geological events.The southwestward thickening of the Turonian sequence is interpreted to result from tilting, and the absence of Coniacian and Santonian sediments in the western part of the study area is probably the result of non-deposition. Seismic truncations show evidence of a widespread inversion phase, the timing of which differs between the structural elements. It started at the end of the Campanian followed by a second pulse during the Maastrichtian, a new finding not reported before. After subsidence during the Maastrichtian and Danian, renewed inversion and erosion occurred at the end of the Danian. Halokinesis processes resulted in thickness variations of chalk units of different ages.In summary, variations in sedimentation patterns in the northern Dutch North Sea relate to the Sub-Hercynian inversion phase during the Campanian and Maastrichtian, the Laramide inversion phase at the end of the Danian, and halokinesis processes. Additionally, the Late Cretaceous sea floor was characterized by erosion through contour bottom currents at different scales and resedimentation by slope failures.