The composition of the continental crust is closely tied to subduction zone magmatism. Elevated oxygen fugacity (fO₂) plays a central role in fostering crystallization of oxide minerals and thereby aids in generating the calc-alkaline trend of iron depletion that characterizes the continents. Along continental margins, arc magmas erupt through continental...
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Stephanie B. Grocke a,b,∗, Elizabeth Cottrell a, Shanaka de Silva b, Katherine A. Kelley c
a Smithsonian