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Late Plio-Pleistocene evolution of the Eurasian Ice Sheets inferred from sediment input along the northeastern Atlantic continental margin - ScienceDirect
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PDF) The Molo Formation, deposited by coastal progradation on the inner Mid-Norwegian continental shelf, coeval with the Kai Formation to the west and the Utsira Formation in the North Sea
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500 m of rapid base level rise along an inner passive margin – Seismic observations from the Pliocene Molo Formation, mid Norway - ScienceDirect
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500 m of rapid base level rise along an inner passive margin – Seismic observations from the Pliocene Molo Formation, mid Norway - ScienceDirect
PDF) The Molo Formation, deposited by coastal progradation on the inner Mid-Norwegian continental shelf, coeval with the Kai Formation to the west and the Utsira Formation in the North Sea
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