60 likes | 158 Views
Yingcai Zheng w/ input from Ru-shan Wu and Thorne Lay University of California, Santa Cruz. Length scales of mantle heterogeneities from seismological perspective. P(k). ? ? ?. Fine scale, ~1km. Large scale ~100s-1000s km. Small/medium scale ~10s km. k.
E N D
Yingcai Zheng w/ input from Ru-shan Wu and Thorne Lay University of California, Santa Cruz Length scales of mantle heterogeneities from seismological perspective P(k) ? ? ? Fine scale, ~1km Large scale ~100s-1000s km Small/medium scale ~10s km k Seismic velocity heterogeneities: Scale issue
logA(x) ϕ(x) Observational geometry: wavefront “distortion” of a teleseismic plane wave Chernov,1950; Tatarskii 1971); Aki (1973) and others; Flatte and Wu (1988); Zheng, Wu, Lay (2007), Zheng and Wu (2008). Incomplete …
Estimated slope is -2.56 for L-curve result in the shaded region
Estimated slope is -1.28 for L-curve result in the shaded region
Implications to CIDER inter-disciplinary investigation • Based on the seismic results: size and strength of the multiscale heterogeneities, likely to be compositional. • Assuming the origin of the heterogeneity,e.g., oceanic crust • long-term evolution of the Earth’s interior: vol. of the subducted oceanic crust retained in the mantle; • layering of the heterogeneity and multiscale spectra of the heterogeneity (CONVECTION) • mixing model of the mantle (PETRO) • Compare with spectra of isotopic ratios along ocean ridges with seismic heterogeneity spectra (GEOCHEM)