Mantle Convection and Surface Expressions. Группа авторов

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3 Seismic Wave Velocities in Earth’s Mantle from Mineral Elasticity

      Johannes Buchen

       Seismological Laboratory, California Institute of Technology, Pasadena, CA, USA

      ABSTRACT

      The propagation of seismic waves through Earth’s mantle is controlled by the elastic properties of the minerals that form mantle rocks. Changes in pressure, temperature, and chemical composition of the mantle as well as phase transitions affect seismic wave speeds through their impact on mineral elasticity. СКАЧАТЬ