Table 2_Crustal assimilation in arc magmas controlled by overriding plate thickness.xlsx
<p>Magmas erupting in arcs range in composition from MgO-rich basalt to MgO-poor rhyolite. This broad compositional range is due to the sequential crystallization and separation of minerals with different chemical compositions from the cooling magma (a process known as fractional crystallizati...
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2025
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