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地幔主要矿物组成与深度分布

已有 691 次阅读 2026-9-30 13:30 |个人分类:地球科学|系统分类:科研笔记

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数据来源

  • Anderson, D. L., & Bass, J. D. (1984). Mineralogy and composition of the upper mantle. Geophysical Research Letters, 11(7), 637–640. https://doi.org/10.1029/GL011i007p00637

  • Ito, E., & Takahashi, E. (1989). Postspinel transformations in the system Mg₂SiO₄–Fe₂SiO₄ and some geophysical implications. Journal of Geophysical Research: Solid Earth, 94(B8), 10637–10646. https://doi.org/10.1029/JB094iB08p10637

  • Irifune, T., et al. (1998). The postspinel phase boundary in Mg₂SiO₄ determined by in situ X-ray diffraction. Science, 279(5357), 1698–1700.

  • Katsura, T., Yamada, H., Nishikawa, O., Song, M., Kubo, A., Shinmei, T., Yokoshi, S., Hirao, N., Mito, T., & Kondo, T. (2003). Post-spinel transition in Mg₂SiO₄ determined by high P–T in situ X-ray diffractometry. Physics of the Earth and Planetary Interiors, 136(1–2), 11–24.

  • Nishiyama, N., Irifune, T., Inoue, T., Ando, J., & Funakoshi, K.-I. (2004). Precise determination of phase relations in pyrolite across the 660 km seismic discontinuity by in situ X-ray diffraction and quench experiments. Physics of the Earth and Planetary Interiors, 143(1–2), 185–199.

  • Sinogeikin, S. V., Katsura, T., & Bass, J. D. (2003). Sound velocities and elastic properties of Fe-bearing wadsleyite and ringwoodite. Journal of Geophysical Research: Solid Earth, 108(B2), 2093.

  • Murakami, M., Ohishi, Y., Hirao, N., & Hirose, K. (2012). A perovskitic lower mantle inferred from high-pressure, high-temperature sound velocity data. Nature, 485, 90–94.

  • Irifune, T., Ismailova, L., & others. (2010). Iron partitioning and density changes of pyrolite in Earth's lower mantle. Science, 327(5962), 193–195.

  • Xu, Y. (2025). Phase relations of bridgmanite, the most abundant mineral in the Earth's lower mantle. Communications Chemistry, 8. 



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