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Fig 1: Small scale folds (crenulations) in a mica-rich fault rock (phyllonite) from the Kvenklubben fault,
Repparfjord, Finnmark (Photograph: E. Torgersen).
Figur 2: A fold with a lot of limestone in Repparfjord, Finnmark. Foto: HJ Kjøll
Figur 3: A LIDAR-photo of the northwestern part of the island Bømlo in Vestland county. You can see a lot
of cracks in the photo
Figur 5: Structure map of the east part of Repparfjord tectonic window in Finnmark. A projection of
layerspilt sandstone in the Saltvann-formation (Yellow circles in the map to the left)
A small-scale quartz porphyroclast that, due to its asymmetry, can be used as a kinematic indicator
within the Kalak Nappe Complex exposed at Markopp, Repparfjord, Finnmark. Photo: G. Viola
Figure 7: A set of composite shear fractures cutting a pegmatite (white area) within a granitic host rock.
The displacement of the pegmatite vein allows geologists to understand what has happened here, a long
time ago. The photo is captured on the island Kalla close to Olkiluoto, SW Finland, where Finnish
authorities are building a deep repository for long-term storage of high-grade nuclear waste. The
structural analysis of who brittle deformation effects the area is important for designing the repository and
for assessing the potential of future seismic activity. Photo: G. Viola.
Structural geology-25-9.pptx
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Structural geology-25-9.pptx

  • 1.
  • 2.
  • 3.
  • 4.
  • 5.
  • 6.
  • 7.
  • 8.
  • 9. Fig 1: Small scale folds (crenulations) in a mica-rich fault rock (phyllonite) from the Kvenklubben fault, Repparfjord, Finnmark (Photograph: E. Torgersen).
  • 10. Figur 2: A fold with a lot of limestone in Repparfjord, Finnmark. Foto: HJ Kjøll
  • 11. Figur 3: A LIDAR-photo of the northwestern part of the island Bømlo in Vestland county. You can see a lot of cracks in the photo
  • 12. Figur 5: Structure map of the east part of Repparfjord tectonic window in Finnmark. A projection of layerspilt sandstone in the Saltvann-formation (Yellow circles in the map to the left)
  • 13. A small-scale quartz porphyroclast that, due to its asymmetry, can be used as a kinematic indicator within the Kalak Nappe Complex exposed at Markopp, Repparfjord, Finnmark. Photo: G. Viola
  • 14. Figure 7: A set of composite shear fractures cutting a pegmatite (white area) within a granitic host rock. The displacement of the pegmatite vein allows geologists to understand what has happened here, a long time ago. The photo is captured on the island Kalla close to Olkiluoto, SW Finland, where Finnish authorities are building a deep repository for long-term storage of high-grade nuclear waste. The structural analysis of who brittle deformation effects the area is important for designing the repository and for assessing the potential of future seismic activity. Photo: G. Viola.