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   <subfield code="u">Key Laboratory of the Earth's Deep Interior, Institute of Geology and Geophysics, Chinese Academy of Sciences, 100029, Beijing, China</subfield>
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   <subfield code="a">Quantitative assessment of the complexity of geological structures in terms of seismic propagators</subfield>
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   <subfield code="c">[LiYun Fu]</subfield>
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   <subfield code="a">How a wave interacts with heterogeneous media has been pursued by many geophysicists. The complexity of subsurface heterogeneities is seismologically a relative concept to wavelengths of seismic waves. A growing perception is that velocity variations, propagation angles, and computational accuracies are closely related at a variety of scales. A tentative strategy to quantitatively evaluate the complexity of subsurface heterogeneous media is presented in this article to see what scales of geological heterogeneities to be captured by waves. We express complex subsurface structures as the slowness- and angular-heterogeneity spectra to quantify velocity contrasts and dipping-angle distributions of complex geological structures. On the other hand, the scaling characteristics of a propagator are measured through dispersion analysis by its angular spectra plotted against refractive indexes and propagation angles, respectively. A parameter termed as imaging efficiency is introduced by associating the geological heterogeneity spectra with the propagator's angular spectra to understand the coherent interference between the medium's heterogeneity and the propagator's scaling characteristics. Furthermore, a complexity coefficient can be defined to evaluate geological complexities in terms of propagators. The application of this strategy is demonstrated to the SEG/EAEG salt model.</subfield>
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   <subfield code="a">Science in China Press and Springer Berlin Heidelberg, 2009</subfield>
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   <subfield code="t">Science in China Series D: Earth Sciences</subfield>
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   <subfield code="t">Science in China Series D: Earth Sciences</subfield>
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