Magmas generated in Earth’s mantle evolve through a complex interplay of crystallisation, mixing, assimilation and volatile exsolution as they ascend through the crust. Hydrous phases, and amphibole ...
SILICATES of the amphibole group are known to decompose endothermically, at temperatures above 600° C, to give a pyroxene and other products 1–3. The composition of the pyroxene and other products is ...
Some results have been hidden because they may be inaccessible to you
Show inaccessible results