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Crustal structures of Eastern Fennoscandia
Tectonophysics, 1991The area of the Eastern Fennoscandian Shield is quite well covered by deep seismic sounding profiles, most of which were shot in the last ten years. In general the velocities of the seismic waves in the crust increase continuously with depth, but intense reflections also indicate the presence of distinct velocity boundaries.
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Crustal Thicknesses of Fennoscandia
1979Pirhonen, S., Bungum, H., Husebye, E. S.
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