In order to understand the characteristics of acoustic wave propagation in rocks within seismic frequency band (<100
Hz), the velocities of longitudinal and transverse waves of four different types of rocks were tested using low-frequency
stress-strain method by means of the physical testing system of rock at low frequency and the experimental data of acoustic
velocities of four different types of rocks at this frequency band were obtained. The experimental results showed that the
acoustic velocities of four different types of rocks increased with the increase of temperature and pressure within the
temperature and pressure ranges set by the experiment. The acoustic velocity of fine sandstone at 50% water saturation
was smaller than that of dry sample. The acoustic velocities of four different types of rocks were different and the velocities
of longitudinal waves of gritstone, fine sandstone, argillaceous siltstone and mudstone increased in turn under similar
conditions and were smaller than those at ultrasonic frequency. Few of existing studies focus on the acoustic velocity at
seismic frequency band, thus, further understanding of the acoustic characteristics at this seismic frequency band still
requires more experimental data.