Thermobarometry provides a critical means of assessing locations of magma storage and
dynamics in the lead-up to volcanic eruptions and crustal growth. A common approach is to …

The physical process of crystal-melt separation is responsible for the accumulation of small
to very large volumes (> 100 km3) of eruptible rhyolitic melt in the shallow crust. Granitic …

Understanding the drivers of the onset, evolution, and end of eruptions and their impact on
eruption style is critical in eruption forecasting and emergency management. The …

With the recognition of multiple crustal cross sections on our planet, the advent of high-
precision geochronology, and the ever-increasing application of geophysical imaging …

Forecast of eruptive activity is a core challenge in volcanology. Here, we present an actual
forecast for the end of the 2021 La Palma eruption. Using continuous GNSS data, we …

Ocean island basalts (OIBs) are generated by mantle plumes, with their geochemistry
controlled by a combination of source composition, temperature, and thickness of overlying …

Eastern Australia encompasses the longest track (~ 2000 km) of age-progressive continental
volcanoes on Earth. These so-called 'central volcanoes' are shield volcanoes considered as …

Understanding the Mesozoic lithospheric mantle beneath South China is challenging,
primarily because mantle-derived magmatic rocks are rare, whereas granitic magmatism is …

Abstract The El Abrigo member of the Diego Hernández Formation (Tenerife, Canary
Islands) represents the final (170 ka) and most voluminous eruption (> 20-km3 DRE) of the …

The depths of crustal reservoirs within volcanic systems may experience transitions over
time. Here, we report the crystal and bulk rock compositions of the shield-forming basaltic …