Abstract
High-pressure phase relations in the system Mg4Si4O12Mg3Al2Si3O12 were investigated at pressures from 10 to 22 GPa and at a temperature of 1000°C. The experimental results indicate that the maximum solubility of enstatite (Mg4Si4O12) in pyrope (Mg3Al2Si3O12) is 80 mol% enstatite at 15 GPa. At pressures between 15 and 19 GPa, the solubility is insensitive to pressure. At 19 GPa, garnet-ilmenite transformation first occurs in enstatite composition. At pressures above 19 GPa, the compositional range of the ilmenite solid solution expands toward pyrope composition with increasing pressure. Based on the present experiments, if pyrolite mantle is assumed, the pyroxene-garnet transformation appears at 350-400 km depth, and garnet + modified spinel and garnet + spinel phase assemblages become stable successively up to ∼ 580 km depth. At greater depths, garnet decomposes to ilmenite + garnet and hence the pyrolite mantle consists of ilmenite + garnet + spinel assemblage.
| Original language | English |
|---|---|
| Pages (from-to) | 168-175 |
| Number of pages | 8 |
| Journal | Physics of the Earth and Planetary Interiors |
| Volume | 49 |
| Issue number | 1-2 |
| DOIs | |
| Publication status | Published - 1987 |
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ASJC Scopus subject areas
- Geophysics
- Space and Planetary Science
- Physics and Astronomy (miscellaneous)
- Astronomy and Astrophysics
Cite this
Ultrahigh-pressure phase relations in the system Mg4Si4O12Mg3Al2Si3O12 . / Kanzaki, Masami.
In: Physics of the Earth and Planetary Interiors, Vol. 49, No. 1-2, 1987, p. 168-175.Research output: Contribution to journal › Article
}
TY - JOUR
T1 - Ultrahigh-pressure phase relations in the system Mg4Si4O12Mg3Al2Si3O12
AU - Kanzaki, Masami
PY - 1987
Y1 - 1987
N2 - High-pressure phase relations in the system Mg4Si4O12Mg3Al2Si3O12 were investigated at pressures from 10 to 22 GPa and at a temperature of 1000°C. The experimental results indicate that the maximum solubility of enstatite (Mg4Si4O12) in pyrope (Mg3Al2Si3O12) is 80 mol% enstatite at 15 GPa. At pressures between 15 and 19 GPa, the solubility is insensitive to pressure. At 19 GPa, garnet-ilmenite transformation first occurs in enstatite composition. At pressures above 19 GPa, the compositional range of the ilmenite solid solution expands toward pyrope composition with increasing pressure. Based on the present experiments, if pyrolite mantle is assumed, the pyroxene-garnet transformation appears at 350-400 km depth, and garnet + modified spinel and garnet + spinel phase assemblages become stable successively up to ∼ 580 km depth. At greater depths, garnet decomposes to ilmenite + garnet and hence the pyrolite mantle consists of ilmenite + garnet + spinel assemblage.
AB - High-pressure phase relations in the system Mg4Si4O12Mg3Al2Si3O12 were investigated at pressures from 10 to 22 GPa and at a temperature of 1000°C. The experimental results indicate that the maximum solubility of enstatite (Mg4Si4O12) in pyrope (Mg3Al2Si3O12) is 80 mol% enstatite at 15 GPa. At pressures between 15 and 19 GPa, the solubility is insensitive to pressure. At 19 GPa, garnet-ilmenite transformation first occurs in enstatite composition. At pressures above 19 GPa, the compositional range of the ilmenite solid solution expands toward pyrope composition with increasing pressure. Based on the present experiments, if pyrolite mantle is assumed, the pyroxene-garnet transformation appears at 350-400 km depth, and garnet + modified spinel and garnet + spinel phase assemblages become stable successively up to ∼ 580 km depth. At greater depths, garnet decomposes to ilmenite + garnet and hence the pyrolite mantle consists of ilmenite + garnet + spinel assemblage.
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UR - http://www.scopus.com/inward/citedby.url?scp=0000187699&partnerID=8YFLogxK
U2 - 10.1016/0031-9201(87)90139-7
DO - 10.1016/0031-9201(87)90139-7
M3 - Article
AN - SCOPUS:0000187699
VL - 49
SP - 168
EP - 175
JO - Physics of the Earth and Planetary Interiors
JF - Physics of the Earth and Planetary Interiors
SN - 0031-9201
IS - 1-2
ER -