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American Mineralogist

Journal of Earth and Planetary Materials

Ed. by Baker, Don / Xu, Hongwu / Swainson, Ian

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Volume 102, Issue 7


Experimental evidence for the survival of augite to transition zone depths, and implications for subduction zone dynamics

Jingui Xu
  • Key Laboratory of High Temperature and High Pressure Study of the Earth’s Interior, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China
  • Hawaii Institute of Geophysics and Planetology, School of Ocean and Earth Science and Technology, University of Hawaii at Manoa, 1680 East West Road, POST Building, Honolulu, Hawaii 96822, U.S.A
  • University of Chinese Academy of Sciences, Beijing 100049, China
  • Other articles by this author:
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/ Dongzhou Zhang
  • Hawaii Institute of Geophysics and Planetology, School of Ocean and Earth Science and Technology, University of Hawaii at Manoa, 1680 East West Road, POST Building, Honolulu, Hawaii 96822, U.S.A
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/ Przemyslaw Dera
  • Hawaii Institute of Geophysics and Planetology, School of Ocean and Earth Science and Technology, University of Hawaii at Manoa, 1680 East West Road, POST Building, Honolulu, Hawaii 96822, U.S.A
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/ Bo Zhang
  • Key Laboratory of High Temperature and High Pressure Study of the Earth’s Interior, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China
  • University of Chinese Academy of Sciences, Beijing 100049, China
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  • De Gruyter OnlineGoogle Scholar
/ Dawei Fan
  • Key Laboratory of High Temperature and High Pressure Study of the Earth’s Interior, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China
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Published Online: 2017-07-17 | DOI: https://doi.org/10.2138/am-2017-5959


(Ca, Mg)-rich clinopyroxenes are abundant in Earth’s upper mantle and subduction zones. Experimental studies on the thermoelastic properties of these minerals at simultaneous high pressure and high temperature are important for constraining of the composition and structure of the Earth. Here, we present a synchrotron-based single-crystal X-ray diffraction study of natural diopside-dominated augite [(Ca0.89Na0.05Mg0.06)(Mg0.74Fe0.11Al0.14Ti0.01)(Si1.88Al0.12) O6.00] at P and T to ~27 GPa and 700 K. The experiment simulates conditions in cold subducting slabs, and results indicate that augite is stable over this pressure and temperature range. A third-order high-temperature Birch-Murnaghan equation was fit with the pressure-volume-temperature data, yielding the following thermoelastic parameters: KT0 = 111(1) GPa, KT0 = 4.1(1), (∂K0/∂T)P = −0.008(5) GPa/K and αT = 4(1)×10−5 K−1 +2(3)×10−8 K−2 T. A strain analysis shows that the compression along the three principal stress directions is highly anisotropic with ε1:ε2:ε3 = 1.98:2.43:1.00. Additionally, high-pressure structural refinements of room-temperature polyhedral geometry, bond lengths and O3-O3-O3 angle were investigated to ~27 GPa at ambient temperature. Pressure dependences of polyhedral volumes and distortion indicate that the substitution of Al3+ for Si4+ significantly changes the compressional behavior of the TO4-tetrahedron in augite. Density calculations of this augite along a subducting slab geotherm suggest that augite as well as other common clinopyroxenes would promote slab stagnations at transition zone depths if they are metastably preserved in significant quantities.

Keywords: Pyroxenes; augite; high pressure and temperature; single-crystal X-ray diffraction; subduction zone

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About the article

Received: 2016-09-16

Accepted: 2017-02-26

Published Online: 2017-07-17

Published in Print: 2017-07-26

Citation Information: American Mineralogist, Volume 102, Issue 7, Pages 1516–1524, ISSN (Online) 1945-3027, ISSN (Print) 0003-004X, DOI: https://doi.org/10.2138/am-2017-5959.

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