A correct description and quantification of the geochemical behaviour of REE+ Y (rare earth
elements and Y) and HFSE (high field strength elements) is a key requirement for modeling …

The purpose of this review study is to reappraise in a more comprehensive form the
thermodynamic principles behind the partitioning of trace elements between clinopyroxene …

Thermobarometry is a fundamental tool to quantitatively interrogate magma plumbing
systems and broaden our appreciation of volcanic processes. Developments in random …

Clinopyroxene is a key fractionating phase in alkaline magmatic systems, but its impact on
metal enrichment processes, and the formation of REE+ HFSE mineralisation in particular, is …

Caldera-forming eruptions, during which large volumes of magma are explosively
evacuated into the atmosphere from shallow crustal reservoirs, are one of the most …

Within subvolcanic plumbing systems, along volcanic conduits and post-eruptive
emplacement, mineral textures and compositions are governed by complex kinetic …

Magmatism is very common in the Okinawa Trough. However, the influence of magmatic
processes, including fractional crystallization and magma mixing, on the petrogenesis of …

Sector-zoned clinopyroxene records kinetic effects imposed by variable degrees of magma
undercooling, ΔT, and can be utilised to track the dynamics of magmatic systems. The …

Understanding the mechanisms responsible for the generation of chemical gradients in high-
volume ignimbrites is key to retrieve information on the processes that control the maturation …

We present kinetic partitioning data for trace cations measured in zoned clinopyroxene
crystals obtained from a variably cooled and decompressed olivine basalt erupted at Mt …