Variation of Nernst partition coefficients (D) between olivine and silicate melts cannot be
neglected when modeling partial melting and fractional crystallization. Published natural …

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

The Yanacocha magmatic field (northern Peru) hosts the largest high sulfidation gold
deposit on Earth. Mineralization is associated with porphyritic intrusions distributed along a …

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 …

The accreted Talkeetna arc, south-central Alaska, is an archetypal example of an intra-
oceanic arc crustal section. Arc-related units include all levels of a lithospheric column, from …

How a volcano has behaved throughout its past is a guide to its future behaviour. Detailed
knowledge of what preceded eruptions from specific volcanoes, and how this can be …

Nernst partition coefficient data between orthopyroxene and silicate melts show variability
for most trace elements which cannot be neglected when designing petrogenetic trace …

Significant petrogenetic processes governing the geochemical evolution of magma bodies
include magma R echarge (including formation of 'quenched inclusions' or enclaves) …

Flood basalts are some of the largest magmatic events in Earth history, with intrusion and
eruption of millions of km3 of basaltic magma over a short time period (∼ 1–5 Ma). A typical …