Stability of Magnesite under the Lower Mantle Conditions
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- Type
- article
- Published
- 1991-01-01
- Cited by
- 36
- References
- 2
- Access
- Open access
- OpenAlex
- https://openalex.org/W2012566560
- Semantic Scholar
- https://api.semanticscholar.org/CorpusID:129855134
Keywords
Magnesite, Compressibility, Mantle (geology), Geology, Volume (thermodynamics)
References
Cited by
- First principles calculations on the high-pressure behavior of magnesite
- Comparative compressibilities of calcite-structure carbonates: Deviations from empirical relations
- The equation of state and high-pressure behavior of magnesite
- Solidus of carbonated peridotite from 10 to 20 GPa and origin of magnesiocarbonatite melt in the Earth's deep mantle
- Thermal equation of state of magnesite to 32 GPa and 2073 K
- Stability of magnesite and its high-pressure form in the lowermost mantle
- Experimental determination of carbon isotope fractionation between graphite and carbonated silicate melt under upper mantle conditions
- Equation of state of magnesite for the conditions of the Earth’s lower mantle
- X-ray diffraction study of magnesite at high pressure and high temperature
- Magnesite formation from MgO and CO2 at the pressures and temperatures of Earth’s mantle
- Experimental investigation of the stability of Fe‐rich carbonates in the lower mantle
- Experimental determination of equilibrium magnesiumisotope fractionation between spinel, forsterite, andmagnesite from 600 to 800 ºC
- A calcite --> aragonite-type phase transition in CdCO3
- Melting of subducted carbonated pelites from 5 to 23 GPa: Alkali-carbonatites, mantle metasomatism, and element recycling
- High-temperature heat capacity of grossular (Ca3Al2Si3O12), enstatite (MgSiO3), and titanite (CaTiSiO5)
- Melting and subsolidus phase relations in the system Na2CO3-MgCO3±H2O at 6 GPa and the stability of Na2Mg(CO3)2 in the upper mantle
- Structural refinements of magnesite at very high pressure
- The system CaCO₃-MgCO₃: experiments and thermodynamic modeling of the trigonal and orthorhombic solid solutions at high pressure and teperature
- Decoupling of Mg–C and Sr–Nd–O isotopes traces the role of recycled carbon in magnesiocarbonatites from the Tarim Large Igneous Province
- The high-pressure behavior of spherocobaltite (CoCO3): a single crystal Raman spectroscopy and XRD study
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