Volcanic systems are swarms of tectonic fractures and basalt volcanoes formed as a result of
plate-pull (as the plates are pulled apart) associated with the mid-ocean ridges and the …

Hot spot–mid‐ocean ridge interactions cause many of the largest structural and chemical
anomalies in Earth's ocean basins. Correlated geophysical and geochemical anomalies are …

The large-scale volcanic lineaments in Iceland are an axial zone, which is delineated by the
Reykjanes, West and North Volcanic Zones (RVZ, WVZ, NVZ) and the East Volcanic Zone …

Abstract The high 3He/4He ratio of volcanic rocks thought to be derived from mantle plumes
is taken as evidence for the existence of a mantle reservoir that has remained largely …

In this paper, we have adopted a modern, cutting-edge methodology to make geoheritage
sites (geosites) available and explorable worldwide, through both immersive and non …

The compositions of volcanic materials are sensitive to physical conditions in the underlying
magmatic system. When basaltic melts are saturated in olivine‐plagioclase‐augite prior to …

This book provides a summary of geodynamic results from Iceland that presently are found
in a great number of scientific articles, but have not been collected before in a book. The …

We present the results of a comprehensive major element, trace element and Sr–Nd–Pb–O
isotopic study of post-glacial volcanic rocks from the Neovolcanic zones on Iceland. The …

Iceland has a unique geology and a dynamic natural landscape which has long attracted a
large number of tourists to the island. Owing to the dynamic geological processes which are …

New Sr–Nd–Pb–Hf data require the existence of at least four mantle components in the
genesis of basalts from the the North Atlantic Igneous Province (NAIP):(1) one (or more likely …