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2 Acta Geophysica Polonica

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Seismic rotation waves related to volcanic, mining and seismic events: Near-field and micromorphic motions

Teisseyre R., Teisseyre K., Moriya T., Palangio P.

Acta Geophysica Polonica

2003

Vol. 51, nr 4

409-431

Rotation and twist waves recorded in Hokkaido (Japan), Ojców and Książ (Poland) and L'Aquila (Italy) bring a new insinght into the features of these motions for volcanic, mining and tectonic events. The rotation seismograph system used at the observatories in Hokkaido differs from that observatories in Poland and Italy. Nevertheless, the results obtained, for all observatories, are compatible. The levels of rotation and twist motions depend distinctly on the back-ground properties of the recording sited. Moreover, at a given recording station we have noticed two different levels of these motions; for some near events the records indicate very small rotation motions, while for other, also near events, these motions are distinctly greater and remain on a similar level as those for records from the distant sources. For the near events the evident differences in magnitudes and character of these motions suggest a distinct relation between the rotation and twist motions and the source mechanism. Similarly, an analysis of records for the volcanic events indicates existence of two kinds of events: for the first group, the rotation components reach the order of magnitude much greater than those for the group, for which the rotation and twist motions are quite negligible. The records related to this group, representing probably the near-surface volcanic explosions, confirm at the same time the reliability of results obtained for the rotation motions belonging to the first group, as the technique of recording and distances remain for both groups the same. The records from several stations give grounds for searching for as influence local structure on rotation and twist motions. The data treatment applied for local events made it possible to separate the recorded motions into the micromorphic and source related parts.

Discussion on the recording of seismic rotation waves

Teisseyre R., Moriya T.

Acta Geophysica Polonica

1999

Vol. 47, nr 4

351-362

The new instrumentation technique permits to record the seismic rotational waves. In the case of a non-ideal elasticity the rotation waves appear due to defect content (the non-symmetric disclinations) in a medium or due to internal structure of a medium (micromorphic or micropolar media). Rotations may be attributed either to distortion from the plane wave state (rigid rotation related to the displacement field) or, more generally, to an independent microdisplacement tensor with rotation and twist-bend components. In this paper we analize the observed examples of records of rotation waves and we discuss the instrumental possibilities to record complex rotation phenomena of a non-rigid type.