Sofia Pechlivanidou
0000-0002-0376-6103
University of Bergen
2 papers found
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Tectono‐sedimentary evolution of high‐displacement crustal‐scale normal faults and basement highs on rifted margins: Klakk Fault Complex and Frøya High, Mid‐Norwegian Margin
From subsurface to surface: a multidisciplinary approach to decoding uplift histories in tectonically‐active karst landscapes
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