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- W4312853919 endingPage "200" @default.
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- W4312853919 abstract "High-pressure silicates and oxides have been found in nature as mineral inclusionsInclusion in diamondsDiamond derived from the Earth’s mantle and as minerals in shocked meteoritesShocked meteorite and impacted terrestrial rocks. These natural high-pressure mineralsHigh-pressure mineral are discussed in this chapter. High-pressure and high-temperature phase relations determined experimentally and by thermodynamic calculation can be used to evaluate pressure and temperature environments where the mantle-derived high-pressure mineralsHigh-pressure mineral were formed. The determined phase relations can also be used for constraining the P and T conditions that the shocked minerals experienced during the shockShock event for the analysis of the impact processes." @default.
- W4312853919 created "2023-01-05" @default.
- W4312853919 creator A5035122094 @default.
- W4312853919 date "2022-01-01" @default.
- W4312853919 modified "2023-09-27" @default.
- W4312853919 title "High-Pressure Minerals from the Earth’s Mantle and in Shocked Meteorites" @default.
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- W4312853919 doi "https://doi.org/10.1007/978-981-19-6363-6_11" @default.
- W4312853919 hasPublicationYear "2022" @default.
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