A large majority of igneous rocks on Earth are formed by a process known as fractional crystallization (summarized in the diagram below). To understand this process, start by imagining a large liquid magma (melt) body. As we cool the magma, mineral phases become stable and crystals start to form. The newly formed minerals are likely …[Read More]
Geochemistry, Mineralogy, Petrology & Volcanology
Welcome to the new GMPV blog!
Welcome to the brand-new blog for the EGU Geochemistry, Mineralogy, Petrology & Volcanology (GMPV) Division! The aim of this blog is to provide a unique space for all mineral geeks, volcanophiles and rocking chemists to tell the world about their latest research and exciting new ideas! The GMPV Division covers a huge range of themes …[Read More]