-
目前主要从事变形流变学以及矿物物理相关方面的工作，具体包括：（1）天然岩石的变形显微构造研究；（2）高温高压实验矿物流变学研究；（3）高压矿物物理性质研究（实验波速）；（4）中深源地震成因机制研究
- 俯冲带中源地震成因机制的实验与观测对比研究,2027-12-31,在研,通过实验与观测，对比研究高温高温条件下不同岩石脆性破裂机制下所产生的地震信号差异
- 俯冲带绿泥石高温高压流变学实验研究,2020-01-21,2022-12-31,结题,通过5GPa Griggs流变仪研究高温高压条件下绿泥石结合体的流变学性质
- 俯冲带叶蛇纹石脱水显微结构及波速研究,2025-01-01,在研,通过同步辐射技术测量高温高压原位条件下叶蛇纹石集合体的波速特征
- 深地科学高温高压实验前沿研究,2025-08-01,在研,突破深地科学高温高压实验关键技术瓶颈，建设由4个中心（成矿过程、大压机、动高压、同步辐射原位探测）组成的相辅相成、互为补充、模拟条件覆盖地壳－地核的深地科学高温高压实验前沿研究中心。
- 暂无内容
- 暂无内容
- hi F., Wang Y.*, Yu T., Zhu L., Zhang J., Wen J., Gasc J., Incel S., Schubnel A., Li Z., Chen T.,Liu W., Prakapenka V. and Jin Z., Lower-crustal earthquake in southern Tibet are linked to eclogitization of dry metastable granulite, Nature Communications (2018), 9, 3483.doi:10.1038/s41467-018-05964-1. (T1, Nature index)
- Liu W., Zhang J.*, Barou F., B-type olivine fabric induced by low temperature dissolution creep during serpentinization and deformation in mantle wedge. Tectonophysics (2018), 722,1-10. doi:10.1016/j.tecto.2017.10.025. (T2)
- Liu, W., Cao Y., Zhang J.*, Zhang Y., Zong K., and Jin Z., Thermo-structural evolution of the val malenco (Italy) peridotite: A petrological, geochemical and microstructural study, Minerals (2020), 10(11), 1-22, doi:10.3390/min10110962. (T3)
- Liu, W., Zhang J., Cao Y.*, and Jin Z., Geneses of Two Contrasting Antigorite Crystal Preferred Orientations and Their Implications for Seismic Anisotropy in the Forearc Mantle, Journal of Geophysical Research: Solid Earth (2020), 125(9), doi:10.1029/2020JB019354. (T1, Nature Index)
- Liu, W., Xu, H.*, Shi F., Decorated dislocations in naturally deformed olivine with C-type fabric: A case study in the Lüliangshan garnet peridotite from the North Qaidam ultrahigh-pressure belt, NW China. Tectonophysics (2021), 814(5). (T2)