Quantifying transient mantle convective uplift: An example from the Faroe-Shetland basin

摘要

The Icelandic mantle plume generated maximum uplift in early Paleogene times. The Faroe-Shetland basin, which fringes the North Atlantic margin of Europe, was close to the center of early Paleogene Icelandic plume activity. Three-dimensional seismic refle