Mg diffusion in forsterite from 1250–1600 °C
نویسندگان
چکیده
منابع مشابه
Melting of Forsterite, Mg<sub>2</sub>SiO<sub>4</sub>, From 9.7 to 16.5 GPa
A multianvil apparatus ha been used to determine th pressure-temperature mel ing curve of forsterite from 9.7 to 16.5 GPa. At 10.1 GPa a singular point occurs that marks the change from congruent melting at lower pressures to incongruent melting (forsterite periclase + liquid) at higher pressures. The melting curve also passes through two invariant points. At one (15.6 GPa, 2310øC), the phases ...
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ژورنال
عنوان ژورنال: American Mineralogist
سال: 2020
ISSN: 0003-004X,1945-3027
DOI: 10.2138/am-2020-7286