Crustal Magmatic System Evolution: Anatomy, Architecture, and Physico-Chemical Processes

The composition of igneous rocks – their minerals, melts, and fluids – reveals the physical and chemical conditions under which magmas form, evolve, interact, and move from the Earth’s mantle through the crust. These magma dynamics affect processes on the surface including crustal growth and eruptive behaviour of volcanoes. By Matteo Masotta (Editor), Christoph Beier (Editor), Silvio Mollo (Editor)

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