Volume 42 Issue 6
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Xu Lili, Jin Zhenmin, Mei Shenghua, 2017. Deformation-DIA Coupled with Synchrotron X-Ray Diffraction and Its Applications to Deformation Experiments of Minerals at High Temperature and High Pressure. Earth Science, 42(6): 974-989. doi: 10.3799/dqkx.2017.078
Citation: Xu Lili, Jin Zhenmin, Mei Shenghua, 2017. Deformation-DIA Coupled with Synchrotron X-Ray Diffraction and Its Applications to Deformation Experiments of Minerals at High Temperature and High Pressure. Earth Science, 42(6): 974-989. doi: 10.3799/dqkx.2017.078

Deformation-DIA Coupled with Synchrotron X-Ray Diffraction and Its Applications to Deformation Experiments of Minerals at High Temperature and High Pressure

doi: 10.3799/dqkx.2017.078
  • Received Date: 2016-11-20
  • Publish Date: 2017-06-15
  • Deformation experiment at high temperature and high pressure is one of the important approaches to understand the rheological properties of minerals in the earth's deep interior. The deformation-DIA (D-DIA) is a newly developed apparatus for deformation experiments at high temperature and high pressure, which is typically capable of generating pressures up to 15 GPa and temperatures up to 2 000 K. The D-DIA coupled with synchrotron X-ray diffraction is mainly used for quantitative studies of rheological properties of materials under high temperature and high pressure. The configuration and operating principle of D-DIA apparatus installed at Brookhaven national lab in USA are summarized in this paper. The in-situ observation of deformation processes using synchrotron X-ray diffraction and mechanical data (e.g., stress, strain and strain rate) analysis are also discussed. This technical development provides an important opportunity to investigate rheological properties of high-pressure phases under the conditions in the earth's deep interior.

     

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