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- W2000869384 abstract "Deep and intermediate earthquakes cannot be explained in terms of slow accumulation and sudden release of stress because relaxation rates in the earth's mantle are such that accumulation of stress over a long period of time does not appear likely. Consequently, sudden volume changes due to phase transitions in the mantle have been suggested as a possible energy source for these earthquakes. However, a phase transition at equilibrium pressure and temperature cannot result in the spontaneous release of energy because the rate of appearance of the new phase is determined by the rate at which energy enters or leaves the system. Thus a sudden release of free energy requires a spontaneous change from the metastable state. Slow currents in the earth's mantle contained between phase discontinuities could generate effects resulting in the transport of a mineral assemblage from one pressure-temperature environment to another. If the pressurevolume changes in these currents are essentially adiabatic the pressuretemperature environment near a phase discontinuity would be favourable for spontaneous phase transitions, even though the environment at the phase discontinuity in the surrounding mantle was that of equilibrium. Thus, the hypothesis that deep and intermediate earthquakes are triggered by sudden volume changes is consistent with thermodynamic considerations." @default.
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- W2000869384 date "1965-11-01" @default.
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- W2000869384 title "Earthquakes resulting from metastable phase transitions" @default.
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- W2000869384 doi "https://doi.org/10.1016/0040-1951(65)90034-x" @default.
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