Elasticity of β-Mg2SiO4 containing 1.2 wt% H2O to 10 GPa and 600 K by ultrasonic interferometry with synchrotron X-radiation
Noda, M., Gwanmesia, G. D., Whitaker, M. L., Chen, H., Inoue, T., Sakamoto, N., and Yurimoto, H. “Elasticity of β-Mg2SiO4 containing 1.2 wt% H2O to 10 GPa and 600 K by ultrasonic interferometry with synchrotron X-radiation.” American Mineralogist 111 (2026): 128137. https://pubs.geoscienceworld.org/msa/ammin/article/111/1/128/654502/Elasticity-of-Mg2SiO4-containing-1-2-wt-H2O-to-10
High-pressure Cr3+ luminescence and Raman spectroscopy of a natural MgAl2O4 spinel to ∼60 GPa
Pease, A., D. Sneed, C. Vennari, and E. F. O’Bannon III. “High-pressure Cr3+ luminescence and Raman spectroscopy of a natural MgAl2O4 spinel to∼ 60 GPa.” Journal of Luminescence 289 (2026): 121634. https://www.sciencedirect.com/science/article/pii/S0022231325005733
Equation of state of Fe-bearing epidote-group minerals determined by X-ray diffraction
Zhang, Xinyue, Ningyu Sun, and Zhu Mao. “Equation of state of Fe-bearing epidote-group minerals determined by X-ray diffraction.” American Mineralogist 111, no. 1 (2026): 108-117. https://pubs.geoscienceworld.org/msa/ammin/article/111/1/108/723890/Equation-of-state-of-Fe-bearing-epidote-group
Redox reactions in subducted CaCO3–Fe–SiO2 as a potential source of superdeep diamond inclusions
Guo, M., Li, X., Mao, Z. et al. Redox reactions in subducted CaCO3–Fe–SiO2 as a potential source of superdeep diamond inclusions. Sci Rep 16, 3618 (2026). https://doi.org/10.1038/s41598-025-33661-9
Pressure-temperature stability and equation of state of staurolite: Implications for the water transport during cold slab subduction
Shijie Huang, Jingui Xu, Dongzhou Zhang, Shanrong Zhang, Yufeng Liu, Yikui Liang, Zimo Li, Wenge Zhou, Dawei Fan, “Pressure-temperature stability and equation of state of staurolite: Implications for the water transport during cold slab subduction,” Lithos 522, 108361 (2026). DOI: 10.1016/j.lithos.2025.108361 https://www.sciencedirect.com/science/article/pii/S0024493725004207?via%3Dihub
Wildfire Produces Transient Minerals: Speciation, Reactivity, and Fate of Iron and Manganese in Surface Soils Post Wildfire
Kang, K., Whelan, E. M., Bone, S., Rowley, M. C., Marcus, M. A., & Peña, J. (2025). Wildfire Produces Transient Minerals: Speciation, Reactivity, and Fate of Iron and Manganese in Surface Soils Post Wildfire. Environmental Science & Technology. https://doi.org/10.1021/acs.est.5c07438
Invisible water in subducted crust: Lawsonite velocity anomalies under mantle conditions
Chen, Sibo, Siheng Wang, Xintong Qi, Man Xu, Tony Yu, Yanbin Wang, and Baosheng Li. “Invisible water in subducted crust: Lawsonite velocity anomalies under mantle conditions.” Proceedings of the National Academy of Sciences 122, no. 49 (2025): e2506548122. https://www.pnas.org/doi/full/10.1073/pnas.2506548122
Viscosity of Dry and Hydrous Diopside Melts at High Pressures: Implications for Upper Mantle Magma Dynamics
Chen, Q., Zhao, B., Yu, T., Ashley, A. W., & Wang, Y. (2025). Viscosity of dry and hydrous diopside melts at high pressures: Implications for upper mantle magma dynamics. Journal of Geophysical Research: Solid Earth, 130, e2025JB032842.
Elasticity of davemaoite as a primary contributor to lower-mantle heterogeneities
Zhou, Wen-Yi, Ming Hao, Wenhao Su, Taehyun Kim, Sibo Chen, Sang-Heon Shim, Dongzhou Zhang, Phuong QH Nguyen, Katherine Armstrong, and Jin S. Zhang. “Elasticity of davemaoite as a primary contributor to lower-mantle heterogeneities.” Science 390, no. 6776 (2025): 935-939. https://www.science.org/doi/10.1126/science.adx8356
Equilibrium Fe isotope fractionation between olivine, pyroxene, spinel and MORB glass: Implications for mantle partial melting to generate MORBs
Nie, Nicole X., Anat Shahar, Peng Ni, Richard W. Carlson, Steven B. Shirey, Corliss K. Sio, Justin Y. Hu et al. “Equilibrium Fe isotope fractionation between olivine, pyroxene, spinel and MORB glass: Implications for mantle partial melting to generate MORBs.” Geochimica et Cosmochimica Acta (2025). Read More