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Showing 1 to 2 of 2 for “"Faroe-Shetland Basin"”.
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The architecture, growth and tectono-stratigraphic significance of rift-oblique lineaments on the NE Atlantic Margin
… the stratigraphic and magmatic evolution of a basin. The NE Atlantic Margin is a volcanic passive margin which has undergone a series of rift events culminating with continental breakup in the Early Cenozoic. From potential field, seismic reflection, seismic refraction and ocean bottom …
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Generation of Buried Transient Landscapes and Residual Depth Anomalies
… seismic reflection surveys from the Faroe-Shetland basin. A regional biostratigraphic and lithostratigraphic framework shows that these transient landscapes recur at intervals of 2–4 million years. Dendritic drainage patterns recovered from these landscapes are disequilibrated and …