An instrument capable of collocated measurement of three perpendicular ground velocity components (two horizontal and one vertical) and three seismic rotation rate components (around two horizontal axes and one vertical) in a high-frequency range of 2-100 Hz. Compared to the older prototypes, the maximum measurable frequency of seismic motions has been considerably increased by suppressing undesirable resonances due to a changed shape of the rigid metal frame of the instrument.
Moreover, the accuracy of the rotational measurement has been significantly increased by using more sensitive geophones at a higher number and in a substantially innovated arrangement.