![Late Plio-Pleistocene evolution of the Eurasian Ice Sheets inferred from sediment input along the northeastern Atlantic continental margin - ScienceDirect Late Plio-Pleistocene evolution of the Eurasian Ice Sheets inferred from sediment input along the northeastern Atlantic continental margin - ScienceDirect](https://ars.els-cdn.com/content/image/1-s2.0-S0277379122000646-gr2.jpg)
Late Plio-Pleistocene evolution of the Eurasian Ice Sheets inferred from sediment input along the northeastern Atlantic continental margin - ScienceDirect
![500 m of rapid base level rise along an inner passive margin – Seismic observations from the Pliocene Molo Formation, mid Norway - ScienceDirect 500 m of rapid base level rise along an inner passive margin – Seismic observations from the Pliocene Molo Formation, mid Norway - ScienceDirect](https://ars.els-cdn.com/content/image/1-s2.0-S0264817217302052-gr15.jpg)
500 m of rapid base level rise along an inner passive margin – Seismic observations from the Pliocene Molo Formation, mid Norway - ScienceDirect
![500 m of rapid base level rise along an inner passive margin – Seismic observations from the Pliocene Molo Formation, mid Norway - ScienceDirect 500 m of rapid base level rise along an inner passive margin – Seismic observations from the Pliocene Molo Formation, mid Norway - ScienceDirect](https://ars.els-cdn.com/content/image/1-s2.0-S0264817217302052-gr3.jpg)
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 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](https://www.researchgate.net/profile/Morten-Smelror/publication/264547759/figure/fig2/AS:654393422647306@1533030958750/Ultra-highresolution-seismic-line-across-the-Molo-Formation-There-are-three-significant_Q320.jpg)
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
![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 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](https://www.researchgate.net/profile/Morten-Smelror/publication/264547759/figure/fig4/AS:654393422667812@1533030958867/The-Molo-Formation-50-km-north-of-Draugen-Although-not-dated-the-unit-between-the-brown_Q320.jpg)
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
![500 m of rapid base level rise along an inner passive margin – Seismic observations from the Pliocene Molo Formation, mid Norway - ScienceDirect 500 m of rapid base level rise along an inner passive margin – Seismic observations from the Pliocene Molo Formation, mid Norway - ScienceDirect](https://ars.els-cdn.com/content/image/1-s2.0-S0264817217302052-gr11.jpg)