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Chinese Journal of High Pressure Physics  > 2018  >  32(1): 010101.
FAN Dawei, LI Bo, CHEN Wei, XU Jingui, KUANG Yunqian, YE Zhilin, ZHOU Wenge, XIE Hongsen. Research Progress of the Equation of State for Garnet Minerals[J]. Chinese Journal of High Pressure Physics, 2018, 32(1): 010101. doi: 10.11858/gywlxb.20170597
Citation: FAN Dawei, LI Bo, CHEN Wei, XU Jingui, KUANG Yunqian, YE Zhilin, ZHOU Wenge, XIE Hongsen. Research Progress of the Equation of State for Garnet Minerals[J]. Chinese Journal of High Pressure Physics, 2018, 32(1): 010101. doi: 10.11858/gywlxb.20170597
shu

Research Progress of the Equation of State for Garnet Minerals

doi: 10.11858/gywlxb.20170597
  • 1.

    Key Laboratory of High-Temperature and High-Pressure of the Earth's Interior, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China

  • 2.

    University of Chinese Academy of Sciences, Beijing 100049, China

  • 3.

    Guizhou Polytechnic of Construction, Guiyang 551400, China

  • Received Date: 23 Jun 2017
  • Rev Recd Date: 07 Jul 2017
    Abstract
  • As an important rock-forming mineral of the rocks in the earth, garnet is one of the most important minerals in the upper mantle, transition zone and (ultra) high pressure metamorphic rocks.The study of its equation of state is therefore of great significance in laying a foundation for constraining the state and chemical composition of the earth interiors, and further understanding the geodynamical processes of the subducted oceanic lithosphere plate and Earth's mantle.This article summarized the recent advances in the studies of the p-V (pressure-cell volume) and p-V-T (pressure-cell volume-temperature) equation of state of the garnet, focusing on the phase stability, the effect of component and hydrogen on the thermal elastic parameters of the garnet at high pressure and high temperature.Finally, the existing problems and prospects of the garnet's equation of state studies were also evaluated.

     

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