The geological development of Greenland spans a period of nearly 4 Ga, from Eoarchaean
to the Quaternary. Greenland is the largest island on Earth with a total area of 2 166 000 km …

Greenland is the largest island on Earth, with 80% of its area covered by a thick ice sheet.
The coastal areas are underlain by variable rocks ranging from Eoarchean to the most …

In 1874, JW Judd, a leading British geologist, wrote:“In the Hebrides I will now show that we
have supplied to us that great geological desideratum–a number of volcanoes so dissected …

Wide-angle shear wave arrivals, converted from compressional to shear waves at crustal
interfaces, enable crustal Vp/Vs ratios to be determined which provide valuable constraint …

Imaging challenges caused by highly attenuative flood basalt sequences have resulted in
the understanding of volcanic rifted continental margins lagging behind that of non-volcanic …

Seismic reflection data and shallow cores from the SE Greenland margin show that rift
basins formed by the mid-to Late Cretaceous in the offshore area near Ammassalik. Here …

This paper presents a summary of the stratigraphy and structure of the Faroese region. As
the Faroese area is mostly covered by volcanic material, the nature of the pre-volcanic …

The Jan Mayen Micro-Continent (JMMC) is the result of two Cainozoic phases of continental
breakup, and subsequent seafloor spreading. The first established a spreading ridge system …

Abstract The Danish North Sea coast is a dynamic sedimentary environment experiencing
erosion, transport and re-deposition of sand along the coast. Because of the natural and …

During the Cretaceous, the CO2 content of the global atmosphere drastically increased in
response to volcanism associated with the disintegration of the former continents. This …