Gijs Henstra
0000-0001-9805-5875
3 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
The evolution of catchment‐depositional system relationships on the dip slopes of intra‐rift basement highs: An example from the Frøya High, Mid‐Norwegian rifted margin
Supradetachment basins in necking domains of rifted margins: Insights from the Norwegian Sea
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