Sentence examples for for mantle conductivity from inspiring English sources

The inversion for mantle conductivity is initiated with a uniform conductivity model.

The derivation of the elements of the Q-matrix by multivariate analysis and their inversion for mantle conductivity in a similar framework as presented above will be the topic of a forthcoming publication.

Since the two side-by-side flying satellites are equivalent to a single satellite for mantle conductivity studies, this result indicates that it is possible to obtain a good estimate of the 3-D mantle conductivity structure even with data from the global net of observatories and a single satellite, i.e. also from recent missions as, in particular, CHAMP.

When using the coefficients for determination of mantle conductivity, periods up to one month correspond to resolving conductivity down to 1200 km or so.

We have presented a scheme to invert satellite magnetic data for a global depth profile of mantle conductivity.

Below 1000 km, the method is unable to resolve lateral variations of mantle conductivity, and only the 1-D average conductivity is recovered.

(a) 1D models of mantle conductivity and (b) 1D model of mantle C-Response induction; (c) 3D conductivity model from the Time Domain approach at the Earth's surface; (d) 3D model of mantle conductivity from the Time Domain approach at a depth of 400 km showing the recovered image of a synthetic anomaly beneath the Pacific Ocean.

This technique has been valued as the most important method for studying mantle conductivity.

We have presented a 3-D frequency domain inversion scheme to invert satellite magnetic data for global mantle conductivity.

Moreover, the inversion results provide a useful initial guess for 3-D mantle conductivity studies with Swarm data (cf. companion papers by Puthe and Kuvshinov, 2013; Velímský, 2013).

On a planetary scale, long-period data (in the period range from few hours to years) from permanent geomagnetic observatories have been traditionally used in 1-D inversions for depth-dependent mantle conductivity structure.