Magma reservoirs play a key role in controlling numerous processes in planetary evolution,
including igneous differentiation and degassing, crustal construction, and volcanism. For …

Large caldera-forming eruptions have long been a focus of both petrological and
volcanological studies; petrologists have used the eruptive products to probe conditions of …

Magmatic processes on Earth govern the mass, energy and chemical transfer between the
mantle, crust and atmosphere. To understand magma storage conditions in the crust that …

The term “ignimbrite” probably encompasses the one of the largest ranges of deposit types
on Earth, associated with the partial to total collapse of explosive eruption columns feeding …

Multistage histories of incremental accumulation, fractionation, and solidification during
construction of large subvolcanic magma bodies that remained sufficiently liquid to erupt are …

In continental-margin subduction zones, basalt magmas spawned in the mantle interact with
the crust to produce a broad spectrum of volcanic arc associations. A distinct style of very …

Worst-case or high-end subduction-related earthquakes and tsunamis of 2004 and 2011 are
painfully fresh in our memories. High-end subduction-related volcanic eruptions have not …

Formation and evolution of the Pannonian Basin as part of the Mediterranean region was
accompanied by eruptions of compositionally diverse magmas during the Neogene to …

Polygenetic volcanoes and calderas produce eruptions of a wide variety of magnitudes,
chemistries, and recurrence times. Understanding the interplay between long-and short-term …

The last supereruption from the Yellowstone Plateau formed Yellowstone caldera and
ejected the> 1000 km3 of rhyolite that composes the Lava Creek Tuff. Tephra from the Lava …