聚焦于岩浆作用的岩石地球化学数值模拟研究，在充分考虑熔体和晶体之间的相对运动和化学反应基础上，引入两相流体力学概念，模拟软流圈中地幔不均匀体对于洋脊岩浆作用的影响，以及俯冲带火山岩浆房喷发过程。

1. 岩浆作用的两相流数值模拟
2. 地幔不均一性
3. 超级火山
   
   

1. 中国科学院人才项目，2023-2028；主持
2. 中国科学院战略性先导科技专项（B），2023-2028；参与

ORCID: orcid.org/0000-0001-7958-7155
第一及通讯（*）作者论文：
截至2025/8/28

1. Chen, H.-B., Liu*, B., Ji*, W.-Q., Zhang, S.-H., Zhao, K., Wu, F.-Y., 2025. Repacking Accelerates High-Silica Melts Extraction: Insights From Microstructural Record and Numerical Modeling. Geophysical Research Letters 52, e2024GL110970. https://doi.org/10.1029/2024GL110970
2. Liu, B., Lee, C.-T., 2021. Fast melt expulsion from crystal-rich mushes via induced anisotropic permeability. Earth and Planetary Science Letters 571, 117113. https://doi.org/10.1016/j.epsl.2021.117113
3. Liu, B., Lee, C.-T., 2020. Large silicic eruptions, episodic recharge, and the transcrustal magmatic system. Geochemistry, Geophysics, Geosystems 21, e2020GC009220. https://doi.org/10.1029/2020gc009220
4. Liu, B., Liang, Y., 2020. Importance of the size and distribution of chemical heterogeneities in the mantle source to the variations of isotope ratios and trace element abundances in mid-ocean ridge basalts. Geochimica Et Cosmochimica Acta 268, 383–404. https://doi.org/10.1016/j.gca.2019.10.013
5. Liu, B., Liang, Y., 2019. Importance of permeability and deep channel network on the distribution of melt, fractionation of REE in abyssal peridotites, and U-series disequilibria in basalts beneath mid-ocean ridges: A numerical study using a 2D double-porosity model. Earth and Planetary Science Letters 528, 115788. https://doi.org/10.1016/j.epsl.2019.115788
6. Liu, B., Liang, Y., 2017a. An introduction of Markov chain Monte Carlo method to geochemical inverse problems: Reading melting parameters from REE abundances in abyssal peridotites. Geochimica Et Cosmochimica Acta 203, 216–234. http://dx.doi.org/10.1016/j.gca.2016.12.040
7. Liu, B., Liang, Y., 2017b. The prevalence of kilometer-scale heterogeneity in the source region of MORB upper mantle. Science Advances 3. http://dx.doi.org/10.1126/sciadv.1701872
8. Liu, B., Liang, Y., Liu, C.-Z., 2024a. Changing shape of mantle heterogeneity by melt migration beneath mid-ocean ridges. Earth and Planetary Science Letters 644, 118925. https://doi.org/10.1016/j.epsl.2024.118925
9. Liu, B., Qi, C., Mitchell, R.N., Lee, C.-T.A., Liu, C.-Z., 2024b. A Model for Melt-Preferred Orientation and Permeabilities in Deformed Partially Molten Peridotites. Geochemistry, Geophysics, Geosystems 25, e2024GC011588. https://doi.org/10.1029/2024GC011588

合作论文：

1. 刘传周, 杨阳, 刘博达, 刘通. (2022). 软流圈地幔成分不均一性的研究进展与意义. 岩石学报, 38(12), 3712-3734.
2. Lee, C.-T., Liu, B. (2021). Thick crust, hydrous magmas, and the paradox of voluminous cold magmatism. Volcanica, 4(2), 227 - 238.
3. Liang, Y., Ji, Z., Liu, B. (2021). What can we learn from REE abundances in clinopyroxene and orthopyroxene in residual mantle peridotites? Contributions to Mineralogy and Petrology, 176(3), 24.
4. Liang, Y., Liu, B. (2018). Stretching chemical heterogeneities by melt migration in an upwelling mantle: An analysis based on time-dependent batch and fractional melting models. Earth and Planetary Science Letters, 498, 275-287.
5. Liang, Y., Liu, B. (2016). Simple models for disequilibrium fractional melting and batch melting with application to REE fractionation in abyssal peridotites. Geochimica Et Cosmochimica Acta, 173, 181-197.