Deformation of olivine-orthopyroxene aggregates at high pressure and temperature: Implications for the seismic properties of the asthenosphere
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文摘
Olivine-orthopyroxene deformation experiments at high-pressure high temperature Olivine CPO vary as a function of the volume of secondary phases. Diffusion creep contribution increases with the volume of secondary phases. Vsh/Vsv in asthenosphere dominated by horizontal flow explained by all compositions Vsh/Vsv in asthenosphere dominated by vertical flow only explained by pyroxene-rich compositions

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