研究生毕业
武汉大学
E-Mail:b8fd67572d3d511cde7ff6b6175f71e6b9fc8d8df91cc46bba70ced1b9b8e9497cb26f5dc9be5ce36a6553df49c9a6d5e0f581420f67f87055cc6c4b955e7ccaa1c47107fec8936627b163c61be6614a45a2e88e4690385eeec101e0a13e5bea84cf2b46276492e35c4a153fc36a28d56a8a8c6e8864be3a53ca652eb00daca3
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Email : b8fd67572d3d511cde7ff6b6175f71e6b9fc8d8df91cc46bba70ced1b9b8e9497cb26f5dc9be5ce36a6553df49c9a6d5e0f581420f67f87055cc6c4b955e7ccaa1c47107fec8936627b163c61be6614a45a2e88e4690385eeec101e0a13e5bea84cf2b46276492e35c4a153fc36a28d56a8a8c6e8864be3a53ca652eb00daca3
Journal:APPLIED GEOPHYSICS Volume:14 Issue:1 ISSN No.:1672-7975 Translation or Not:no Date of Publication:2017-01-01
Pre One:On effective characteristic of Rayleigh surface wave propagation in porous fluid-saturated media at low frequencies
Next One:Comparative analysis on spatiotemporal pore pressure evolution under surface-wave perturbations
