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The earthquake relieved compressional pressure between the Eurasian tectonic plate and the Indian section of the Indo-Australian Plate, which subducts (underthrusts) the Eurasian Plate.
The earthquake and its aftershocks were the result of rock fracturing that relieved compressional pressure between the Eurasian Plate and the Arabian Plate, which subducts (underthrusts) under the Eurasian Plate at an average rate of 0.94 inch (24 mm) per year.
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In rock salt phase, beginning from zero pressures and at high pressures, compressional wave velocity v l increases while to that shear wave velocity v s decreases.
In ZB phase, beginning from zero pressures and at high pressures, compressional wave velocity v l increases while to that shear wave velocity v s decreases.
An additional hint at the role of the pressure is the considerable compressional component of the wave magnetic field.
We discuss how both transverse and compressional waves are affected by inhomogeneous pressure and temperature by examining the wave spectra.
The permanent deformation was obtained at elevated temperature under pressure and the viscoelastic compressional behaviors were observed, characterized by a distinct apparent modulus change in glass transition temperature region.
Since the total field (H: green in the plot) changed, these seem to have been compressional in nature, although no clear pressure pulses were visible in the solar wind.
The compressional wave velocities are plotted against pressure in Figure 3 and against temperature in Figure 4. Figure 3 Plot of the measured V p of quartz aggregate versus pressure at 25°C. Figure 4 Plot of the measured V p of quartz aggregate against temperature at 0.5 GPa.
The compressional velocities increased rapidly up to a pressure of 0.3 GPa.
As the confining pressure increased to 50 MPa, compressional and shear wave velocities increased by less than 10%%.
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