Stress-forecasting: a viable alternative to earthquake prediction in a dynamic Earth

被引:16
作者
Crampin, S [1 ]
机构
[1] Univ Edinburgh, Dept Geol & Geophys, Grant Inst, Edinburgh EH9 3JW, Midlothian, Scotland
来源
TRANSACTIONS OF THE ROYAL SOCIETY OF EDINBURGH-EARTH SCIENCES | 1998年 / 89卷
关键词
anisotropic poro-elasticity; cracks; fracture criticality; modelling deformation; self-organised criticality; shear-wave splitting;
D O I
10.1017/S0263593300007057
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Self-organised criticality of the crust appears to make deterministic earthquake prediction of time, place and magnitude of individual large earthquakes inherently impossible. This closes one line of approach to mitigating earthquake hazards. This paper suggests that a viable alternative to earthquake prediction is monitoring the build-up of stress before a large earthquake can occur. A new understanding of rock deformation allows stress changes to be monitored with seismic shear-wave splitting (seismic birefringence). With a suitable monitoring installation, this would allow the stochastic proximity of impending earthquakes to be recognised so that earthquakes could be forecast in the sense of recognising that crustal deformation was preparing for a large earthquake. Such stress-forecasting is not prediction, but, in many circumstances, a possible forecast crescendo of increasing urgency is exactly what is needed to best mitigate hazard to life and property.
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页码:121 / 133
页数:13
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