Pressure is one of the key variables that controls magmatic phase equilibria. However,
estimating magma storage pressures from erupted products can be challenging. Various …

Sector-zoned clinopyroxene is common in igneous rocks, but has been overlooked in the
study of magmatic processes. Whilst concentric zoning is commonly used as a record of …

Crystals formed prior to a volcanic event can provide evidence of processes leading to and
timing of eruptions. Clinopyroxene is common in basaltic to intermediate volcanoes …

The majority of basaltic magmas stall in the Earth's crust as a result of the rheological
evolution caused by crystallization during transport. However, the relationships between …

Clinopyroxene–liquid geothermobarometry is a widely used tool for estimating the
conditions under which mafic magmas are stored before they erupt. However, redox …

The magmatic architecture and physicochemical processes inside volcanoes influence the
style and timescale of eruptions. A long-standing challenge in volcanology is to establish the …

Isothermal and undercooling experiments were conducted on one of the most primitive
trachybasalts from Mt. Etna volcano in order to examine the crystallization mechanisms …

The Xiarihamu mafic-ultramafic intrusion is situated in the East Kunlun Orogenic Belt (E-
KOB), northern Tibetan Plateau, China, with Ni-Co sulfide mineralization mainly in …

Undercooling and crystallization kinetics are recognized increasingly as important
processes controlling the final textures and compositions of minerals as well as the …

Syneruptive magma mixing is widespread in volcanic eruptions, affecting explosivity and
composition of products, but its evidence in basaltic systems is usually cryptic. Here we …