Abstract
References
Sorry, not available.
Click the PDF button.
Information
Rupture directivity is the important parameter in estimating damage due to earthquakes. However, the traditional
momenttensor inversion technique cannot resolve the real fault plane or the rupture directivity.Toovercome these limitations,
wehave developed anewinversion algorithm to determine themoment tensor solution and the rupture directivity for moderate
earthquakes, using the waveform inversion technique in the frequency domain. Numerical experiments for unilateral and
bilateral rupture models with various rupture velocities confirm that the method can resolve the ambiguity of the fault planes
and the rupture directivity successfully. To verify the feasibility of the technique, we tested the sensitivity to velocity models,
which must be the most critical factor in practice. The results of the sensitivity tests show that the method can be applied even
though the velocity model is not perfect. If this method is applied in regions where the velocity model is well verified, we can
estimate the rupture directivity of a moderate earthquake. This method makes a significant contribution to understanding the
characteristics of earthquakes in those regions.
Rupture directivity is the important parameter in estimating damage due to earthquakes. However, the traditional
momenttensor inversion technique cannot resolve the real fault plane or the rupture directivity.Toovercome these limitations,
wehave developed anewinversion algorithm to determine themoment tensor solution and the rupture directivity for moderate
earthquakes, using the waveform inversion technique in the frequency domain. Numerical experiments for unilateral and
bilateral rupture models with various rupture velocities confirm that the method can resolve the ambiguity of the fault planes
and the rupture directivity successfully. To verify the feasibility of the technique, we tested the sensitivity to velocity models,
which must be the most critical factor in practice. The results of the sensitivity tests show that the method can be applied even
though the velocity model is not perfect. If this method is applied in regions where the velocity model is well verified, we can
estimate the rupture directivity of a moderate earthquake. This method makes a significant contribution to understanding the
characteristics of earthquakes in those regions.
Click the PDF button.
- Publisher :Korean Society of Earth and Exploration Geophysicists
- Publisher(Ko) :한국지구물리물리탐사학회
- Journal Title :Geophysics and Geophysical Exploration
- Journal Title(Ko) :지구물리와 물리탐사
- Volume : 12
- No :1
- Pages :114~120


Geophysics and Geophysical Exploration






