Theory of the Earth

نویسنده

  • Don L. Anderson
چکیده

The densities and seismic velocities of rocks are relatively weak functions of temperature, pressure and composition unless these are accompanied by a drastic change in mineralogy. The physical properties of a rock depend on the proportions and compositions of the various phases or minerals-the mineralogy. These, in turn, depend on temperature, pressure and composition. In general, one cannot assume that the mineralogy is constant as one varies temperature and pressure. Lateral and radial variations of physical properties in the Earth are primarily due to changes in mineralogy. To interpret seismic velocities and density variations requires information about both the stable phase assemblages and the physical properties of minerals.

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تاریخ انتشار 2003