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 …

Recharges of magma underneath basaltic volcanoes can occur as precursory events prior to
an eruption but are not always revealed in geophysical data streams or erupted lavas …

Fusion crusts form during the atmospheric entry heating of meteorites and preserve a record
of the conditions that occurred during deceleration in the atmosphere. The fusion crust of the …

Petrogenetic models of martian magmas reflect the compositional, thermal, and
geodynamical evolution of its interior. Most models for shergottite meteorites, which sampled …

Crystals are direct witnesses of intricate journeys of magma transfer and storage through
Earth's mantle and crust. Crystals thus provide windows into processes that are physically …

Nano-magnetite is a potential archive for biosignatures and paleoenvironmental proxies in
hydrothermal systems. However, sulfidic diagenesis at hydrothermal conditions potentially …

We investigated the early stages of olivine crystal growth via in situ seeded experiments in a
single plagioclase-hosted melt inclusion, using a heating stage microscope. Each …

When magmas erupt at the surface, they may have undergone many changes since their
inception. While olivine drives some of these changes through crystallization and …

Chondrules, the major constituent of chondrites, are millimeter‐sized igneous objects
resulting from the crystallization of silicate liquids produced by the partial or complete …

Abstract The Southern Volcanic Zone (SVZ) in Chile is an active continental arc with a
complex history of volcanism, where a range of magmatic compositions have been erupted …