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The laboratory study of the physical properties of rocks and minerals under conditions which reproduce as faithfully as possible those which prevail within the Earth's interior - with particular current emphasis upon the measurement under conditions of high pressure, pore pressure and temperature of elastic wave speeds and attenuation;
Application of similar experimental methods in the characterisation of non-geological materials such as ceramics and metals;
The interpretation of such measurements in terms of the fundamental physics and chemistry of crystalline and partially molten materials, and fluid-saturated porous media;
Application of well-understood laboratory data in the interpretation of seismological models for the spatial variation of density, elastic wave speeds and attenuation;
Constraints imposed by such interpretation upon the constitution and evolution of the Earth.
The laboratory study of the physical properties of rocks and minerals under conditions which reproduce as faithfully as possible those which prevail within the Earth's interior - with particular current emphasis upon the measurement under conditions of high pressure, pore pressure and temperature of elastic wave speeds and attenuation;
Application of similar experimental methods in the characterisation of non-geological materials such as ceramics and metals;
The interpretation of such measurements in terms of the fundamental physics and chemistry of crystalline and partially molten materials, and fluid-saturated porous media;
Application of well-understood laboratory data in the interpretation of seismological models for the spatial variation of density, elastic wave speeds and attenuation;
Constraints imposed by such interpretation upon the constitution and evolution of the Earth.
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Physics of the Earth and Planetary Interiorspp.107160, (2024)
crossref(2023)
Historical Records of Australian Scienceno. 1 (2022): 54-63
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