Most of the high-resolution studies investigating the past variability of the deep North Atlantic
circulation are focused on recent timescales, but little is known for periods older than the last …

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 …

Volcanism in lceland appears to have been confined to volcanic systems throughout its
history. During Late-Pleistocene and Holocene times some 41 volcanic systems have been …

This paper provides a review of geological, geophysical, and geochemical studies for three
geothermal zones of Hengill Volcano, Iceland: Nesjavellir, Hellisheidi, and Hveragerdi. We …

We compile a new geochemical database (Icelandic Volcanic rocks Isotopic Database, IVID)
which includes previously reported 87 Sr/86 Sr, 143 Nd/144 Nd, 176 Hf/177 Hf, 206 Pb/204 …

Geothermal systems are complex environments where geochemical signatures are
controlled by the influx of deep mantle fluids as well as near-surface processes that result …

We studied the seismic velocity structure beneath the Krafla central volcano, NE Iceland, by
performing 3‐D tomographic inversions of 1453 earthquakes recorded by a temporary local …

The origin of the Quaternary silicic rocks in Iceland is thought to be linked to the thermal
state of the crust, which in turn depends on the regional tectonic settings. This simple model …

Networks of seismographs of high sensitivity have been in use in the vicinity of active
volcanoes in Iceland since 1973. During this time, 21 confirmed eruptions have occurred …

The interaction between a rift zone and a mantle plume leads to exceptional situations in
Iceland where the island is 1.5 wider than expected, given the North-Atlantic spreading rate …