Use this URL to cite or link to this record in EThOS: http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.694217
Title: Tidal triggering of earthquakes
Author: Bucholc, Magda
ISNI:       0000 0004 5990 3415
Awarding Body: Ulster University
Current Institution: Ulster University
Date of Award: 2015
Availability of Full Text:
Full text unavailable from EThOS. Thesis embargoed until 01 Nov 2017
Abstract:
Since tidal forces deform the Earth's crust with completely predictable stresses, the role of the Earth tides in triggering seismicity has long been investigated. The results of these investigations have, however, been inconclusive. Tidal triggering has been found to be non-existent or small (still not statistically significant) for strike-slip faults. On the other hand, a tide-earthquake has been observed in hydrothermal or magmaaffected areas and for reverse faults in the oceanic settings where the amplitude of tidal stresses is the largest. Here, we examine the effect of tidal stresses on earthquake occurrence in Southern California using three novel approaches. First, we analyse the difference in seismicity rates at times of positive and negative tidal Coulomb stresses/stress rates; for that, we resolve the tidal stresses/stress rates on failure planes assumed to be controlled by the orientation of their nearest geological structures. We find the earthquake behaviour with respect to tidal influence statistically non-random only in close proximity to tidal extremes. A particularly strong tidal signal is observed for reverse fault type events. Along with the significant increase in earthquake rates around tidal Coulomb stress maxima, we observe that the strength of the tidal correlation is closely related to the amplitude of the tidal stresses. Second, we look at the response of aftershocks to tidal stresses. Based on the 1992 Mw 7.3 Landers and 1999 Mw 7.1 aftershock activity, we demonstrate that the probability of a fault failure due to tidal oscillations is strongly affected by earthquake-induced static stress changes. Accordingly, earthquakes in regions of increased static stresses are more consistent with tidal triggering than events in areas of static stress decrease. Third, we examine the relationship between the effect of tidal maximum compressional stresses on earthquake timing and the orientation of regional tectonic stress.
Supervisor: Not available Sponsor: Not available
Qualification Name: Thesis (Ph.D.) Qualification Level: Doctoral
EThOS ID: uk.bl.ethos.694217  DOI: Not available
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