Biotite (sensu lato) is a widespread rock‐forming mineral in magmatic rocks that can be
stable in a broad range of pressure and temperature, but appropriate biotite thermometers or …

The peninsular and insular Italy are punctuated by Quaternary volcanoes and their rocks
constitute an important aliquot of the Italian Quaternary sedimentary successions. Also away …

We introduce a new approach, based on machine learning, to estimate pre‐eruptive
temperatures and storage depths using clinopyroxene‐melt pairs and clinopyroxene‐only …

We present new thermometers and barometers based on clinopyroxene–liquid equilibria
specific to alkaline differentiated magmas. The new models were calibrated through the …

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

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 …

To understand the processes that made the 2010 eruption of Merapi much larger and more
explosive than most dome-forming eruptions of the past century, we investigated the …

There is considerable evidence for continuing, late-stage interaction between the magmatic
system at Merapi volcano, Indonesia, and local crustal carbonate (limestone). Calc-silicate …

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

Water and carbon dioxide are the most abundant volatile components in terrestrial magmas.
As they exsolve into magmatic vapour, they promote magma buoyancy, accelerating ascent …