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- W2162223441 abstract "New (revised) data on thermodynamic properties of 60 substances are calculated by extrapolating their compressibilities and calorific properties up to 4000 K and 1 Mbar. Stability of pyrrhotite throughout the mantle supports Goldschmidt's idea about a sulphide zone between the mantle and the core. Such a zone could serve as a primary source of ores. Volatile H2O and H2S are stable throughout the mantle. Some hydrocarbons decompose into a mixture of methane and carbon over a wide range of pressures and temperatures. Natural oil may be regarded as a mixture of metastable hydrocarbons. FeO does not dissociate into a mixture of Fe2O3 and Fe at high pressure and temperature. Alkali-free carbonate magmas may arise in the mantle. The greater the proportion of iron-silicates in the mantle, the more probable is the existence of a ferrous-ferric garnet zone at great depth." @default.
- W2162223441 created "2016-06-24" @default.
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- W2162223441 date "2007-04-30" @default.
- W2162223441 modified "2023-09-25" @default.
- W2162223441 title "Revised and supplemented data on Gibbs' free energies of substances at the parameters of the Earth's mantle" @default.
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- W2162223441 doi "https://doi.org/10.1002/gj.3350240202" @default.
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