Article ID Journal Published Year Pages File Type
4694867 Tectonophysics 2006 10 Pages PDF
Abstract

The stress-aligned shear-wave splitting observed throughout most of the crust is a three-dimensional function of the effective elastic anisotropy of distributions of fluid-saturated grain-boundary cracks and preferentially oriented pores. Fluid-saturated microcracks are highly compliant and crack geometry responds readily to changes in stress. Monitoring with shear-wave splitting allows the accumulation of stress before earthquakes to be recognised and the time and magnitude of the impending earthquake to be stress-forecast. Such increases in stress have been observed some 15 times with hindsight and one successful real-time stress-forecast. Here we report a further with-hindsight stress-forecast in Northern Iceland, where increases of time-delays implying stress accumulation are observed before a 4.9 earthquake at two seismic stations at epicentral distances of 50 km and 92 km. There are, however, two anomalies. Changes in shear-wave polarisations at the nearest station appear to be due to migration of shear-wave source earthquakes, in a uniform anisotropic symmetry, into ray path directions with different anisotropic shear-wave polarisations. Such directional changes in shear-wave polarisations are occasionally observed above small earthquakes and may be misinterpreted as structural or temporal changes in anisotropy. A further anomaly is that the station at 92 km displays variations in time-delays, but a station just 4 km farther away on the other side of a major fault appears to be in the stress shadow of the fault and does not display temporal variations despite having adequate source data.

Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Earth-Surface Processes
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