Finding the isentropic density of perovskite: Implications for iron concentration in the lower mantle

10.1029/96gl03951 · 1997 · Geophysical Research Letters

Orson L. Anderson

5 EOS records from this paper

Phase	Composition	T_ref	V₀	K₀ (GPa)	K′	EOS model	Method note	Origin
Bridgmanite	(Mg,Fe)SiO3	—	—	—	3.900	unknown	—	Cited
Why this differs from similar rows: Cites Stixrude et al. [1992] in a compilation table (Table 1) of thermoelastic parameters; other rows in this table cite different original studies.
Bridgmanite	(Mg,Fe)SiO3	—	—	—	4	unknown	—	Cited
Why this differs from similar rows: Cites Wang et al. [1994] in the same compilation table (Table 1); other rows cite different original studies.
Bridgmanite	(Mg,Fe)SiO3	—	—	—	3.900	unknown	—	Cited
Why this differs from similar rows: Cites Anderson & Masuda [1994] in the same compilation table (Table 1); other rows cite different original studies.
Bridgmanite	(Mg,Fe)SiO3	—	—	—	4	unknown	—	Cited
Why this differs from similar rows: Cites Utsumi et al. [1995] in the same compilation table (Table 1); other rows cite different original studies.
Bridgmanite	(Mg,Fe)SiO3	—	—	—	4	unknown	—	Cited
Why this differs from similar rows: Cites Funamori et al. [1996] in the same compilation table (Table 1); other rows cite different original studies.