Abstract
Tiltmeter observations with application of horizontal pendulums have been carried out for 40 years in the Geodynamic Laboratory in Książ. Long-term observations have not indicated any correlation of these data with meteorological or seasonal phenomena. Following an epoch of fast azimuth changes, a gradual compensation process took place, excluding the effect of gravitational creep of the rock massif. An assumption was made that the observed large changes of the equilibrium azimuths of the horizontal pendulums that result from tectonic tilt of the foundation blocks. Multiannual tiltmeter observations allowed to determine the temporal characteristics and amplitude tectonic effects. Intervals of strong tectonic activity in the rock massif of the Świebodzice Depression last from several days to over ten weeks and are separated by several tens of hours of low activity. Amplitude of the rock massif deformation reaches values from over ten to several tens of amplitudes of the tidal signal, i.e. up to several hundreds of micrometres. Water-tube tiltmeters (WT) launched in 2003 have confirmed the characteristics of tectonic effects and their incidental occurrence. Beside the tilt effects, WT have enabled to confirm vertical movement of the foundation blocks. Geological investigations in the Świebodzice Depression have indicated the presence of a numerous faults separating particular blocks in the rock massif. The presence of this fault system favours the dislocation of foundation blocks, which results in a quake-less relaxation of tectonic stresses and absence lack of seismic activity in the Świebodzice Depression. Foundation blocks separated by faults combined with the multiscale measurement system of WTs form a natural detector of regional tectonic activity, allowing to determine with micrometric resolution the representative function of tectonic activity in the rock massif of the Świebodzice Depression.
Highlights
The Geodynamic Laboratory of the Space Research Centre of the Polish Academy of Sciences (GL) is ORFDWHG LQ WKH XQGHUJURXQG FRUULGRUV XQGHU WKH .VLąĪ Castle [1,2,3]
Elaboration of the observation series from water-tube tiltmeters (WT) and determination of TAF derivatives allowed to discover the temporal and amplitude relationships between the URFN PDVVLIDFWLYLW\RIWKH ĝZLHERG]LFH'HSUHVVLRQDQG the strong (>=4 Mag) seismic events in the Fore-Sudetic Monocline [22]. Comparative analysis of both types of phenomena lead to a conclusion that strong seismic shocks take place only at specific stages of tectonic DFWLYLW\RIWKHĝ'URFNPDVVLI6WDJHVRIWHFWRQLFDFWLYLW\ of the rock massif are described by the TAF functions and their derivatives (Fig. 2)
The results of comparative analysis made for 26 seismic events allowed to conclude that the processes in the rock massif which precede seismic events follow a repeatable succession of rules. This observation allowed to include in the description of the process at which the rock massif becomes ready for a seismic shock, the temporal and amplitude rules consisting of a number of precedents
Summary
The Geodynamic Laboratory of the Space Research Centre of the Polish Academy of Sciences (GL) is ORFDWHG LQ WKH XQGHUJURXQG FRUULGRUV XQGHU WKH .VLąĪ Castle [1,2,3]. Elaboration of the observation series from WTs and determination of TAF derivatives allowed to discover the temporal and amplitude relationships between the URFN PDVVLIDFWLYLW\RIWKH ĝZLHERG]LFH'HSUHVVLRQDQG the strong (>=4 Mag) seismic events in the Fore-Sudetic Monocline [22]. Comparative analysis of both types of phenomena lead to a conclusion that strong seismic shocks take place only at specific stages of tectonic DFWLYLW\RIWKHĝ'URFNPDVVLI6WDJHVRIWHFWRQLFDFWLYLW\ of the rock massif are described by the TAF functions and their derivatives (Fig. 2).
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