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

Oxygen is the most abundant element in the Earth's crust, mantle, and fluids and therefore its
isotopic composition provides robust constraints on magma genesis. Application of oxygen …

Whether a magma body is able to produce eruptions and at what frequency remains a
challenging problem in volcanology as it involves the nonlinear interplay of different …

Open-system processes have a large capacity to modify magma compositions during
differentiation. Obtaining the rates of such processes is essential to understanding and …

Thermal reactivation of locked crystal mushes in the upper crust is a fundamental step
towards volcanic eruptions of crystal-rich magmas. Models of such reactivation events …

Early Jurassic sheet-like intrusions (sills and dykes) are abundant in the Karoo Basin in
South Africa, and were emplaced as a part of the Karoo Large Igneous Province. Here we …

The Magma Chamber Simulator quantifies the impact of simultaneous recharge,
assimilation and crystallization through mass and enthalpy balance in a multicomponent …

Volcanism is the surface expression of extensive magmatic systems, with their intrusive
counterpart representing~ 80% of the total magma budget. Our knowledge of igneous …

Abstract The undeformed 564 Ma Sept Iles layered intrusion (Quebec, Canada) is a large
igneous body of c. 20 000 km3. From the base to the top, it consists of a Layered Series …

Abstract The Magma Chamber Simulator (MCS) is a thermodynamic model that computes
the phase, thermal, and compositional evolution of a multiphase–multicomponent system of …