Chao‐Yang Guo

Rodingite‐Derived Melt as a Recipe for Ultra‐Calcic Magmas

Abstract Rodingite is a high‐CaO rock formed by Ca‐rich fluid metasomatism on mafic protoliths. It typically occurs within serpentinite and represents an often‐overlooked constituent of the altered oceanic lithosphere that may be subducted into the mantle. However, the fate of ro...