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- W156947803 abstract "Seismic tomography is like a photography taken by a camera with deformed and blurred lenses. Amplitudes and shapes of seismic patterns derived at tomographic images are often strongly biased with respect to real structures in the Earth. In particular, tomography usually provides continuous velocity distributions, while the major velocity changes in the Earth often occur on first order interfaces. While working with noisy data, one has to apply strong damping which makes impossible retrieving realistic amplitudes of anomalies. Uneven ray sampling may cause variable damping effect: within one model, one may obtain overand underdamped solutions in different parts of the study area. Lack of some ray orientations may cause smearing of seismic patterns. Due to these and other reasons, quantitative values reported in most tomographic studies, although supported by pseudo-formal criteria (e.g. trade-off curves), do not often represent the reality." @default.
- W156947803 created "2016-06-24" @default.
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- W156947803 date "2010-05-01" @default.
- W156947803 modified "2023-09-26" @default.
- W156947803 title "FM&TI (Forward Modeling & Tomographic Inversion) approach in passive and active seismic studies" @default.
- W156947803 hasPublicationYear "2010" @default.
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