Equations of State for High Pressure Phases.
نویسندگان
چکیده
منابع مشابه
Equations of state of the high-pressure phases of a natural peridotite and implications for the Earth’s lower mantle
To help determine the chemical composition of the Earth’s mantle, we characterised the high-pressure mineral assemblage of an undepleted natural peridotite—thought to be representative of the Earth’s upper-mantle—to 107 GPa using high-resolution X-ray diffraction. At lower-mantle conditions, the peridotite transforms to the assemblage 76 (F 2)% (Mg0.88Fe0.05 2 + Fe0.01 3 + Al0.12Si0.94)O3 ortho...
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ژورنال
عنوان ژورنال: The Review of High Pressure Science and Technology
سال: 2001
ISSN: 0917-639X,1348-1940
DOI: 10.4131/jshpreview.11.55