
- Annu. Rev. Earth Planet. Sci. 2003. 31:30328 doi: 10.1146/annurev.earth.31.091602.113555
- C. R. Geoscience 335 (2003) 2335 Geodynamics / Godynamique
- Inversion of Surface Waves: Barbara Romanowicz
- Short scale heterogeneity in the lowermost mantle: insights from PcP-P and ScS-S data
- Best Practice in Earthquake Location Using Broadband Three-component Seismic Waveform Data
- The eects of the theoretical formalism and data selection on mantle models derived from waveform tomography
- Res. Lett. 6, 731 (1979); P. M. Cassen, S. J. Peale, R. T. Reynolds, ibid. 7, 987 (1980); S. W. Squyres,
- atoms diffusing rapidly among the six sites. In contrast to the 2V clusters, the larger 3V clusters are active for H2 dissociation (Fig. 2c).
- process is irreversible. Sonication of any of the bundle, tubular, and even sheet-like assemblies
- Geophys. J. Int. (2007) 171, 206222 doi: 10.1111/j.1365-246X.2007.03465.x GJISeismology
- Three-Dimensional Structure at the Base of the Mantle Beneath
- The three-dimensional shear velocity structure of the mantle from the inversion of body, surface and higher-mode waveforms
- GEOPHYSICAL RESEARCH LETTERS, VOL. 28, NO. 6, PAGES 1107-1110, MARCH 15, 2001 Can we resolve 3D density heterogeneity in the
- Geophys. J. Int. (2002) 150, 162179 On the resolution of density anomalies in the Earth's mantle
- of legumes and other organisms9 detailed literature on the various steps in
- The 3D shear velocity structure of the mantle from the inversion of
- Nature Macmillan Publishers Ltd 1998 letters to nature
- An Observation of PKJKP: Inferences on Inner Core Shear Properties Barbara Romanowicz,
- JOURNAL OF GEOPHYSICAL RESEARCH, VOL. , NO. , PAGES 1?? , On the origin of complexity in PKP travel time data.
- Geophys. J. Int. (2007) 170, 460467 doi: 10.1111/j.1365-246X.2007.03399.x GJITectonicsandgeodynamics
- Inner core anisotropy inferred by direct inversion of normal mode spectra
- Z .Physics of the Earth and Planetary Interiors 119 2000 3756 www.elsevier.comrlocaterpepi
- environments is unlikely for a hydrothermal system. There are no facies or thickness trends that indicate the existence of local sources
- the inhomogeneous plasma of the Jovian magneto-sphere and, in general, are not in charge equilibrium
- The eect of DQ on PKP(AB3DF) travel time residuals and possible implications for inner core structure
- Supplementary Methods This supplementary material provides detailed information on how we estimate