By Richard D. Miller, John H. Bradford, Klaus Holliger
Published by way of the yank Geophysical Union as a part of the Geophysical improvement sequence, quantity 15.
Advances in Near-surface Seismology and Ground-penetrating Radar (SEG Geophysical advancements sequence No. 15) is a set of unique papers through well known and revered authors from all over the world. applied sciences utilized in the applying of near-surface seismology and ground-penetrating radar have noticeable major advances within the final a number of years. either equipment have benefited from new processing instruments, elevated desktop speeds, and an elevated number of applications.
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Additional info for Advances in Near-surface Seismology and Ground-penetrating Radar, Volume 15
J. Millero, 1973, Compressibility of water as a function of temperature and pressure: Journal of Chemical Physics, 59, 5529–5536. , and L. A. Gallardo, 2009, Cross-gradients joint 3D inversion with applications to gravity and magnetic data: Geophysics, 74, no. 4, L31–L42. Gallardo, L. , 2007, Multiple cross-gradient joint inversion for geospectral imaging: Geophysical Research Letters, 34, L19301. Gallardo, L. , and M. A. Meju, 2003, Characterization of heterogeneous near-surface materials by joint 2D inversion of DC resistivity and seismic data: Geophysical Research Letters, 30, 1658.
CRm)T (equation 1) is a nonlinear function of frequency and earth properties, equation 1 must be linearized by Taylor-series expansion to employ the matrix theory: JDx ¼ Db, (2) where Db½¼ b À cR (x0 ) is the difference between measured data and model response to the initial estimation; c R(x0) is the model response to the initial S-wave velocity estimates, x0; Dx is a modiﬁcation of the initial estimation; and J is the Jacobian matrix with m rows and n columns (m . n). The elements of the Jacobian matrix are the ﬁrst-order partial derivatives of c R with respect to S-wave velocities.
Meju, 2003, Characterization of heterogeneous near-surface materials by joint 2D inversion of DC resistivity and seismic data: Geophysical Research Letters, 30, 1658. ———, 2004, Joint two-dimensional DC resistivity and seismic travel time inversion with cross-gradient constraints: Journal of Geophysical Research — Solid Earth, 109, B03311. ———, 2007, Joint two-dimensional cross-gradient imaging of magnetotelluric and seismic traveltime data for structural and lithological classiﬁcation: Geophysical Journal International, 169, 1261–1272.