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The amplitude of a phase reflected off the inner core also suggests that it must have a finite rigidity and thus be a solid. Shock wave experiments have shown that the major constituents of both the inner and outer core must comprise elements of an atomic number greater than 23, such as iron, nickel, vanadium, or cobalt. Of these elements, only iron is present in sufficient abundance in the solar system to form the major part of the core. Again, by considering solar system abundances, it appears that the core should contain about 4% nickel.
23 24 CHAPTER 2 Another indicator of lower crust composition is the elastic deformation parameter Poisson’s ratio, which can be expressed in terms of the ratio of P and S wave velocities for a particular medium. 35. Lower values are characteristic of rocks with high silica content, and high values with mafic rocks and relatively low silica content. For example, beneath the Main Ethiopian Rift in East Africa (Fig. , 2005). 28. The higher ratios beneath the rift are attributed to the intrusion and extensive modification of the lower crust by mafic magma (Fig.
If the lower crust is wet, basaltic rocks would occur in the form of amphibolite. If mixed with more silicic material, this would have a seismic velocity in the correct range. , 2003). 23 24 CHAPTER 2 Another indicator of lower crust composition is the elastic deformation parameter Poisson’s ratio, which can be expressed in terms of the ratio of P and S wave velocities for a particular medium. 35. Lower values are characteristic of rocks with high silica content, and high values with mafic rocks and relatively low silica content.
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