Discovering mineral behavior in the hidden Earth: Preface
Youjun Zhang
Geoscience Frontiers ›› 2025, Vol. 16 ›› Issue (1) : 101964.
Discovering mineral behavior in the hidden Earth: Preface
M.F. Guo, X. Li, X. Li, Z. Liu, L. Li, D. Wu, Q. Zhou. Decarbonization of siderite in the water-rich upper mantle. Geosci. Front., 16 (1) (2025), Article 101930,
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Y. Huang, M. Hou, H. Liu. A first-principles study of helium diffusion in aragonite under high pressure up to 40 GPa. Geosci. Front., 16 (1) (2025), Article 101931,
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J. Ma, N. Cai, D. Wang. Elasticity of epidote at high pressure and its implications for the velocity anomaly in subduction zone. Geosci. Front., 16 (1) (2025), Article 101933,
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J. Song, L. Sun, H. Zhang, X. Duan, Z. Guan, L. Zhang, X. Feng, W. Yang, H. Liu, M. Yang, Y. Li, D. Yang, Z. Wang, J. Yang, W. Yang, T. Sekine, Y. Zhang, Z. Zhao, Z. Wu. The Hugoniot curve and sound velocity of forsterite to 1200 GPa. Geosci. Front., 16 (1) (2025), Article 101917,
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M. Xie, J. Fu, A.B. Belonoshko. Equation of state and thermodynamic properties of liquid Fe-O in the Earth’s outer core. Geosci. Front., 16 (1) (2025), Article 101847,
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Y. Xu, Y. He, S. Sun, W. Zhang, W. Dai, D. Kim, H. Li. Viscosities of hcp iron alloys under Earth’s inner core conditions. Geosci. Front., 16 (1) (2025), Article 101935,
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J. Yang, S. Fu, J. Liu, J. Lin. Compressional and shear wave velocities of Fe-bearing silicate post-perovskite in Earth’s lowermost mantle. Geosci. Front., 16 (1) (2025), Article 101915,
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H. Zeng, M. Ma, Y. Li, J. Zhang, H. Guan, X. Li. The effect of antigorite dehydration on velocity structure and water migration in subduction zones. Geosci. Front., 16 (1) (2025), Article 101923,
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X. Zhang, L. Dai, H. Hu, M. Hong, C. Li. Constraints on the spin-state transition of siderite from laboratory-based Raman spectroscopy and electrical conductivity under high temperature and high pressure. Geosci. Front., 16 (1) (2025), Article 101918,
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X. Zhao, M.R. Muir, M. Lv, Z. Zhang, X. Bao, X. Liu. Stabilizing inverse ringwoodite with defects, and a possible origin for the 560-km seismic discontinuity. Geosci. Front., 16 (1) (2025), Article 101896,
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