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Volume 29 Issue 5
Dec 2015
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Chinese Journal of High Pressure Physics  > 2015  >  29(5): 329-336.
LI Ying, DU Jian-Guo, XIE Chao, ZHOU Zhi-Hua. Effect of Temperature on Fe-Mg Partition of Garnet during the High Pressure and High Temperature Metamorphism of Pelitic Rock[J]. Chinese Journal of High Pressure Physics, 2015, 29(5): 329-336. doi: 10.11858/gywlxb.2015.05.002
Citation: LI Ying, DU Jian-Guo, XIE Chao, ZHOU Zhi-Hua. Effect of Temperature on Fe-Mg Partition of Garnet during the High Pressure and High Temperature Metamorphism of Pelitic Rock[J]. Chinese Journal of High Pressure Physics, 2015, 29(5): 329-336. doi: 10.11858/gywlxb.2015.05.002
shu

Effect of Temperature on Fe-Mg Partition of Garnet during the High Pressure and High Temperature Metamorphism of Pelitic Rock

doi: 10.11858/gywlxb.2015.05.002
  • 1.

    Key Laboratory of Earthquake Prediction, Institute of Earthquake Science, China Earthquake Administration, Beijing 100036, China

  • 2.

    Institut für Mineralogie und Kristallchemie, Universität Stuttgart, Azenbergstrasse 18, D-70174 Stuttgart, Germany

  • 3.

    China Earthquake Networks Center, Beijing 100045, China

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  • Author Bio:

    LI Ying(1978—), male, doctor, associate professor, major in fluid geochemistry and experimental geochemistry.E-mail:subduction6@hotmail.com

    Abstract
  • The effects of temperature on Fe-Mg compositions of garnet in a natural pelitic system were studied experimentally at temperatures from 700 to 780 ℃ and pressures from 2.1 to 2.9 GPa.The garnets formed in the run products were mainly characterized by magnesian and ferreous compositions.The contents of pyrope and almandine are more than 88%(mass fraction) in all the garnet particles analyzed, whereas grossular and spessartine are less than 12%.The concentrations of FeO and MgO of garnet in the run products show significant linear relationship with experimental temperatures but which is not observed with pressures.The results determine the Fe-Mg partition trend with temperature in a natural pelitic rock with complex chemical compositions, which is useful for the identification of metamorphic temperature for eclogite facies rocks with a pelitic protolith composition.

     

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