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Volumn 143, Issue 2, 2000, Pages 295-301
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Structures, compressibilities and relative stabilities of the α, β and γ phases of Mg2SiO4 deduced from an electron-gas ionic hamiltonian
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Author keywords
Geochemistry; Mantle; Mantle discontinuities; Mineralogy; Phase transitions; Thermodynamics
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Indexed keywords
CRYSTAL STRUCTURE;
FORSTERITE;
MANTLE CHEMISTRY;
MANTLE PROCESS;
PHASE TRANSITION;
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EID: 0033739878
PISSN: 0956540X
EISSN: None
Source Type: Journal
DOI: 10.1046/j.1365-246X.2000.01242.x Document Type: Conference Paper |
Times cited : (5)
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References (51)
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